Chapter 3. Report of Exposure of Coalition Forces Resulting from the Fallout of the Bombings of Iraqi Chemical, Biological, and Nuclear Facilities (Group II)
There were serious concerns expressed prior to the Persian Gulf War about the fallout that would be caused by the bombing of Iraqi chemical, biological, and nuclear weapons production facilities, storage depots, and bunkers. Certainly these bombings were a necessary part of the conflict, but the consequences as well as the necessity must be acknowledged.
U.S. military doctrine warns that, according to its calculations, the use of a nerve agent against a target area of no more than a dozen hectares (a hectare is about 2.47 acres) can, under certain weather conditions, create a hazard zone downwind of up to 100 kilometers in length. Within this downwind area, friendly military units would have to take protective measures.[1] The amount of agent and materials targeted during the Coalition bombings in Iraq exceeded the amounts cited in the example above certainly by multiples and possibly by orders of magnitude.
The dispersal of the chemical agents and other hazardous substances is controlled by factors such as topography, wind velocity, direction, temperature, precipitation, vertical temperature gradient and atmospheric humidity. These factors will all contribute to the size and type of dispersal pattern which will be observed.[2] Unclassified U.S. satellite imagery confirms that debris from the Coalition bombings was upwardly dispersed, rather than downwardly dispersed as would occur in offensive use, causing chemical agents to be carried by upper atmospheric currents and distributing "trace amounts" of chemical fallout over "down weather" positions. Material distributed from the destruction of the ammunition bunkers and storage depots also traveled upward and outward as confirmed in videotaped records of the destruction of these bunkers obtained by Committee staff. These concerns relating to the fallout from the destruction of these materials were expressed by several credible sources as noted below:
1. As a result of these concerns prior to the war, several of the U.S. national laboratories were consulted and/or prepared reports for the U.S. Army, the US Air Force, and the Department of Energy, advising of the hazards which were associated with bombing these facilities.[3]
2. Prior to the war, Soviet chemical weapons expert 1. Yevstafyev publicly advocated withholding information from the Coalition forces on chemical weapons and military facilities supplied by Moscow to Iraq, on the grounds of national security. "Strikes on chemical and biological weapons facilities on Iraq's territory could rebound on us and cause damage to the population of our country." [4]
3. On February 4, 1991, media sources reported that General Raymond Germanos, a spokesperson for the French Ministry of Defense, confirmed that chemical fallout -- "probably neurotoxins" -- had been detected in small quantities, "a little bit everywhere,". from allied air attacks of Iraqi chemical weapons facilities and the depots that stored them.[5]
4. In late July, 1993, the Czech Minister of Defense confirmed that a Czechoslovak Federative Republic military chemical decontamination unit assigned to an area near the Saudi-Iraqi border had detected the chemical nerve agent Sarin in the air during the early stages of the Gulf War. In this unit, 18 of 169 individuals are believed to be suffering from Gulf War illnesses.[6] While the report goes to some length to refute any allegations of the detection being the result of a direct chemical attack, it does defend the ability of the Czech chemical detection equipment to irrefutably confirm traces of chemical warfare agents. Further, the U.S. government, in the November 10, 1993, briefing only referenced the detection of the nerve agent Sarin (GB) by the Czech forces on January 19, 1991. The Czech document, however, states that both Sarin and Yperite (HD) were detected that day. The fact that multiple agents were detected in measurable airborne concentrations suggests that the agents may have emanated from fallout from Coalition bombings of Iraqi chemical weapons plants or storage bunkers, or from a direct mixed agent attack.
The Czechoslovak Chemical Defense Unit in the Persian Gulf and
the Results of
the Investigations of the Military Use of Poisonous Gases.
This section contains the main body of the translated Czech government report, prepared by the Czech Ministry of Defense in response to requests from Members of the Congress of the United States. Following this translation of the report are related accounts from independent sources.
The unit of 169 Czechoslovak military specialists was dispatched into the Gulf on the basis of an agreement between the governments of the Czech and Slovak Federative Republic (CSFR) and the government of the Kingdom of Saudi Arabia (KSA) regarding their activities and the conditions of their stay in Saudi Arabia This Agreement was signed in Prague on November 19, 1990 and amended in Riyadh on November 22, 1990. The Federal Assembly of the CFSR ratified this Agreement. Resolution 97 was modified by an amendment by the Federal Assembly, authorizing the government of the CFSR to accept a provision of the agreement to permit the crossing of the international borders between the Kingdom of Saudi Arabia and Kuwait. The Government gave its approval through Resolution 71, dated January 31, 1991.
By executive order of the Commander of the Northern Region of the Ministry of Defense of the Kingdom of Saudi Arabia, the unit was assigned on the 22nd of December, in accordance with Article IV of the Agreement, to the military configuration of that region. As of January 1, 1991, the two chemical defense platoons were assigned to the 4th and 20th Brigades of the Army of the Kingdom of Saudi Arabia The remainder of the unit was assigned to the base camp and to the headquarters.
Dislocation and strategic command of the unit was completely within the power of the Army of Saudi Arabia Colonel Jan Valo, commander of the unit, provided specific assignment orders. His duty was to assure that in the course of fulfilling their duties, no Czechoslovak law or basic standard of international law was violated
Beginning on January 27, 1991, the two chemical defense platoons were assigned to the Kingdom of Saudi A Arabia brigades, crossing the border into Kuwait They participated actively in assuring the anti-chemical defenses of the allied units during their execution of the operational plan. On February 5, 1991, the unit was supplemented, bringing its total numbers to 198 people.
The Czechoslovak anti-chemical defense unit primarily performed the following tasks:
1. Anti-chemical defense of the headquarters of the northern region
troops located in the area of King Khalid Military City;2. Anti-chemical defense of the 4th and 20th Brigades of the
Kingdom of Saudi Arabia;3. In the case of chemical attack of personnel, provide on their behalf
facilities for chemical treatment and decontamination.
A part of the anti-chemical defense provisions was continuous chemical intelligence and surveillance, with the objective to identify the use of poisonous substances, provide data for alerting forces, and assist commanders in their decision-making.
During the period after the commencement of the war on January 17, 1991, borderline concentrations of poisonous substances were identified in the air by our chemical surveillance. In the Commanders Report, coveting the antichemical defense battalions' activities during the period from January 1, 1991 until February 28, 1991, it specifically stated.
" During this period borderline life-threatening concentrations of the chemical agents yperite [HDI] and sarin [GB] were identified several-times in both areas of the brigades and in King Khalid Military City (i.e., in the military encampment where the unit was stationed) probably the result of the an Allies' air attacks on the storage facilities of chemical ammunition in the territory of Iraq." This information had been published at the time in the Czechoslovak media."
This aforementioned fact was confirmed by members of the battalion, chemical defense specialists who evaluated and ordered measures for personal protection, (see Attachments - pages from the book of the Operations Unit of the General Command of the Czechoslovak Army in Prague, record #56), and all means of anti-chemical defenses were employed. After about two hours the alert was called off when repeated confirmation tests provided negative results.
The concentrations found, "0. 002 grams of yperite per cubic meter and 0. 003 mg per liter of an unspecified poisonous substance,"[later identified by DOD as Sarin] are at the border of the maximum permitted threshold concentration affecting human organisms. These, however, were only one-time positive results from chemical surveillance which were not confirmed by anyone from the other participating countries. This was supported by the report on January 31, 1991:
"Since January l9th, the Czechoslovak unit has not found any other chemical substances."
The Czechoslovak anti-chemical defense unit had at its disposal all modern chemical surveillance and control technology. These we able to identify borderline levels (7evels that do not affect the functions of human organisms) of suspected toxic substances and they can differentiate the nerve agents, such as satin, from "V" agents.
The assertion that the chemicals were of very low concentrations that do not even cause temporary or minute changes in human organisms can be supported by the following facts:
1. The results of the aforementioned surveillance;
2. No signs of exposure to toxic materials were traced to personnel
on site (toxic nerve agents, like sarin,cause instant reactions; for
example: myosis. In the case of yperite, the first clinical signs of
poisoning usually appear within 4 to 6 hours after exposure);3. None of the personnel present had any later effects (related to exposure).
All of the chemical specialists were professional soldiers (there were 56 of them assigned over the length of the conflict). They are all graduates of military colleges and in middle schools with a chemical defense major, and according to the curriculum, worked with highly toxic substances both in the laboratories and infield training. The training of anti-chemical specialists with selected types of poisonous materials had been conducted practically since the beginning of the anti-chemical defense program in 1956 until February 1990, when such training was halted because of complaints of destruction of the environment from environmental protection movements and the mayors of communities.
The anti-chemical defense specialists who had undergone this training are professionals, and they are able to identify the presence of toxic materials in the terrain, on military equipment, and in the air within the sensitivity ranges of the instruments used. Therefore, there is a high probability that the identified presence of poisonous materials is an objective analysis. At the same time, concentrations that am used at chemical field exercises avid in laboratories are several times higher than the concentrations that were measured in the Persian Gulf
It has been proven that military use of chemical weapons by Iraq did not occur and any such fact would have already have been subjected to extensive investigation by agencies of word peace organizations. One can consider that the data measured could have had origins from industrial facilities or even storage facilities of chemical ammunition that were hit by allied bombardment This is supported by a report of the unit's commander, by my statements, and by other direct participants. All members of the unit were equipped with the most modem means of protection against toxic substances. They were fully comparable with the current world standard. Any kind of exposure by these types of toxic substances would manifest itself immediately or in a very short time, and nothing of this kind has been reported. Latent damage, if it can even be considered in this group, would surely have been uncovered during exit examinations.
On the basis of the abovementioned facts, one can conclude that the event cannot in any was be connected with the use of chemical weapons or their use in battlefield activities, and harm to the Czechoslovak anti-chemical defense unit due to the military use of toxic substances could not have occurred.
These conclusions also are supported by health care specialists. Neither at the time of identification of the toxic substances, nor later, was any member of the unit put under medical care as a result of exposure at this event. All members of the unit were subjected to a complex examination in military hospitals after their return from the Persian Gulf -- primarily in the Central Military Hospital in Prague. Even there, no serious changes caused by demanding climatic conditions or by exposure to toxic substances were identified
Many veterans of the Persian Gulf conflict later participated in, and still participate in, activities of the unit in the Czech Republic Army in Yugoslavia. Even at the time of their departure, no one mentioned any problems.
Despite this, as of 31 August 1993, military doctors had examined 18 Persian Gulf veterans who suffered certain health problems, and three of them remain under a doctor's supervision. So far, in their cases, nothing has been identified beyond routine 'problems related to similar long-term stays abroad.
Other Related Information:
On October 8 1993, U.S. Senate staff interviewed Joseph Boccardi, who initially came forward with information about the detection of chemical agents by the Czechoslovak chemical detection unit prior to the release of the Czech report quoted above. According to this witness, a former member of the U.S. Army assigned to the 1st Cavalry Division as an M1A1 tank crewmember (driver/loader/gunner); he was injured when he fell off of a tank during his service in the Gulf War. He was sent to a medical holding area in northern Saudi Arabia. While there, he was befriended by a lieutenant assigned to the holding unit (Lt. Babika). The lieutenant came to him one day and told him to come along with him.
According to Mr. Boccardi, he and the lieutenant drove about 15-20 minutes to a facility that he was told had been used as a Saudi basic training camp. Mr. Boccardi described the facility as beautiful and palace-like (near King Khalid Military City). Once inside, the lieutenant began speaking a foreign language, which Mr. Boccardi believed to be Russian to two soldiers armed with AK-47s standing at the top of a staircase. The soldiers answered. The lieutenant explained that he was speaking Czech and that these soldiers were also Czech.
Mr. Boccardi said that he and lieutenant went into a room where there were about nine soldiers, smoking, drinking vodka, and playing cards, He learned that they were a NBC (nuclear, biological, chemical) team. He asked someone there "if we were kicking their butts so bad, why didn't they hit us with chemicals?" At that, everyone in the room got quiet and the Czech colonel spoke in "broken English" for the first time. He said, according to Mr. Boccardi, "they did hit us with chemicals." According to the Czech colonel, a SCUD hit where they were staying. As soon as they learned that the Patriot had missed the SCUD, they put on their chemical gear and went out onto a balcony near the railing. The Czech colonel said they detected traces of Sarin and another gas, which Mr. Boccardi believed, began with the letter T.
According to Mr. Boccardi, the Czech colonel said that he called U.S. command officials about the result of their tests. He, the Czech colonel, said that he was told not to say anything about it. The colonel also said that he later heard that a number of the soldiers in the area developed skin rashes shortly after this incident.
After this pan of the conversation, the individuals discussed in general terms why they were not supposed to discuss the incident. This Czech colonel was identified as the commanding officer of this unit.
On December 5, 1993, according to published press reports, Jean Paul Ferrand, a logistics officer with the French contingent, told Senator Richard Shelby that nerve agents and mustard agents were detected on January 24 or 25, 1991, in an area south of King Khalid Military City. According to an Agency France Press report on that date, Ferrand said that two chemical weapons alarms went off when a storm blew wind from Iraq. Ferrand was also attributed as having said that special badges worn on the troop protective suits also registered the presence of chemical weapons.[7]
On Monday, March 28, 1994, Committee staff were contacted by a member of the 371st Chemical Company, located in Greenwood, South Carolina. This individual said that during the Gulf War, he served with the 1st platoon of this unit in the vicinity of King Khalid Military City (KKMC). According to this individual and several other members of his platoon interviewed by Committee staff, two days after an Iraqi Scud missile warhead had exploded in the desert his platoon was sent to a site in the desert a few miles south of KKMC to train with the Czech chemical detection team that had conducted initial tests. They also were trained on the Czech equipment. According to two additional members of the platoon who trained with the Czech team, and were interviewed by Committee staff on April 4, 1994 in the Army Reserve Center in Greenwood, South Carolina, the Czech colonel who commanded the unit had told them that his unit had detected measurable quantities of chemical nerve agent immediately after the Scud attack Unit members were not able to " determine the exact date of the incident, but believe it was sometime in mid to late-January 1991.
The members of the unit described the facility where the Czechoslovak team lived as the "glass palace." They believed that it had previously been used as a Saudi military engineering training facility. The members of the U.S. unit who trained with the Czechs, all NBC specialists, said that the Czech equipment appeared to be more reliable than their own.
The unit Executive officer and first sergeant, while not present during the training mission, confirmed that they too were aware of the training, the missile attack, and the reported detection of the chemicals. The unit first sergeant said that this information had been recorded in the unit's logs, but that he received a message to send the logs to Washington, D.C. for historical purposes shortly after they returned from the Persian Gulf.
When asked if their unit did biological agent testing after incoming missiles had detonated, members of the unit said that they had no biological agent testing capability. While there were several other NBC units in the area, they were unaware of any unit that was conducting biological agent tests.
Finally, the unit said that they had been deployed on several occasions to decontaminate the buses and other vehicles that were used to transport Iraqi enemy prisoners of war to detention facilities.
One member of the unit estimated that as many as 85% of the members of this unit are currently suffering from many of the symptoms associated with Gulf War Syndrome.
U.S. Unofficial Reports of Downwind Exposure Due to Coalition Bombings of Iraqi Chemical and Biological Facilities.
1. During the early phases of the air war, there was extensive media coverage of the coalition bombing of Iraqi chemical, biological, and nuclear facilities. ABC News reported that on January 27, 1991, near the Saudi-Kuwaiti border, elements of the 82nd Airborne Division went through a chemical alert drill that was more than an exercise. According to ABC News coverage, their sensors actually registered traces of chemicals in the air; the result, it appeared, of allied bombing of chemical plants in Iraq. A U.S. medical corpsman told reporters, "When the Air Force bombers hit all the gas places there in Iraq, there's a lot of contamination in the air. Some may have filtered down and set these things off. They're very, very sensitive."[8]
2. Brian Martin, of Niles, Michigan, a Gulf War veteran of the 37th Airborne Combat Engineer battalion, 20th Airborne Brigade, 18th Airborne Corps, arrived in Saudi Arabia on October 8, 1990. According to Martin, in late January 1991, while assigned to an area between Rafha and Naryian about six miles south of the Iraqi border, he recorded in his journal and on videotape that chemical "false alarms" were going off almost every day. At first, according to Martin, the alarms were explained as being caused by vapors coming off the sand. Later, since the alarms kept going off and the troops no longer believed that they were being caused by the vapors, Martin said he was informed by both his battalion commander and the battalion NBC NCO that the alarms were sounding because of "minute" quantities of nerve agent in the air, released by the coalition bombing of Iraqi chemical weapons facilities. The troops were assured that there was no danger.
Mr. Martin believes that he witnessed a Patriot intercept of an incoming SCUD missile between Khafji and Wadi Al Batin during the air war period. He was also given the anti-chemical warfare medication pyridostigmine bromide, and suffered some adverse side effects. He says the drug made him jittery and made his vision "jiggle." Since returning from the Saudi Arabia, Mr. Martin has experienced memory loss, swollen and burning feet, joint disorders, muscle weakness, heart palpitations, shortness of breath, rashes, fatigue, headaches, insomnia, bleeding from the rectum, chronic coughing, running nose, burning eyes, and uncontrollable shaking on his right-side extremities.[9]
3. Mr. Troy Albuck, former anti-tank platoon leader with the 82nd Airborne Division, reported to Committee staff that this unit was told that the chemical alarms were going off because of what was drifting down from the Coalition bombings. He explained that his understanding of the situation was that "it was a lot like the effect of gasoline fumes," in that non-lethal exposure was not harmful and would be counteracted by fresh air. [10]
4. Another source who requested confidentiality reported that he was located approximately 40 miles due east of King Khalid Military City (KKMC), when at one position, every M-8 alarm went off -- over 30 at once. The date was between January 20th and February 1, 1991. The NBC NCO radioed in that a nerve agent plant had been bombed about 150 miles away. The source recalled that they were told to take no action and they did not. [11]
Weather Reports, Climatic Information, and Imagery Smoke Plume Data
Operation Desert Storm
Weather reports during this period were censored by the U.S. and Saudi governments. But environmental groups monitoring an oil spill in the Persian Gulf confirm that the winds were at times blowing from the northwest to the southeast. The chemical and biological warfare agent production plants heavily bombed by the coalition forces during this period are located in Iraq to the north and northwest of coalition troop deployments along the Saudi-Iraqi and Saudi Kuwaiti border.[12]
As cited above, the dispersal of chemical agents and other hazardous substances is controlled by other factors in addition to wind direction and velocity, such as topography, temperature, precipitation, vertical temperature gradient, and atmospheric humidity. These factors all contribute to the size and type of dispersal that will be observed.
In March 1992, the U.S. Air Force Environmental Technical Application Center published a compendium of the weather during Operation Desert Shield and Operation Desert Storm. The following is a summary of relevant data for January 17, 1991 through March 2, 1991, excerpted from Gulf War Weather. The report documents the changing weather conditions, detailing the wind and rain patterns that could easily have delivered chemical and biological agents to coalition troop emplacements. On many dates, this report notes the smoke and dust from the bombings and from the burning oil wells. The notation of visible smoke plumes is not intended to depict the actual fallout from the bombed chemical, biological, and nuclear facilities, but rather too generally reflect the direction of movement of debris from the bombings.
Gulf War Weather
17 January 1991
There were extensive early morning clouds over the entire area. These clouds gradually moved southward during the day as their bases raised to 8, 000 feet. Broken to overcast high clouds from the approaching frontal system begin to move in after 1200Z, quickly spreading over the entire area with ceilings from 20,000 to 25,000 feet. The high cloud base thickened and lowered to 10,000 to 15,000 feet by the end of the day.
Winds were from the south or southwest at 6-20 knots, becoming southeasterly after 1200Z and 3-12 knots after sunset.
Early morning visibility were as low as 3,200 meters with patchy ground fog in west central Iraq. Blowing sand and suspended dust reduced visibility to 3,200 meters during the afternoon on the Saudi Arabia - Iraq border.
High temperatures were 13-22 degrees Celsius, lows 6-10 degrees celsius.
18 January 1991
The entire area was covered by clouds with bases at 10,000-15,000 feet. These quickly lowered to 3,000 feet and, in some places, to as low as 1,500 feet. The western part of the area began clearing in the afternoon, but 200 foot ceilings formed throughout the area by the end of the day. Clouds were layered to 30,000 feet from central Iraq to southeastern Kuwait.
Light rain fell throughout the area beginning as early as 0500Z and lasting past 1800Z in eastern Iraq.
Winds were east to southeasterly at 5-15 knots.
Visibilities were 5 km in morning ground fog and 3,200 meters in rain. After the rain passed, visibilities were as low as 4,800 meters in haze and fog, falling to 1,600 meters by the end of the day.
High temperatures were 16-22 degrees C; lows, 8-13 degrees C.
19 January 1991
High pressure was centered in central Iraq and central Saudi Arabia The stationary frontal system over the area become active when an upper-air disturbance crossed it. A low pressure cell developed and moved the front southward.
The entire area was covered with low clouds with bases at 100-200 feet. By 1200Z the northern part, including Baghdad had cleared Ceilings in the southern section rose briefly a midday to 1,000- 1,500 feet, then returned to 500- 1,000 feet for the rest of the day. After sunset the clouds spread northward into the Baghdad area w ere ceilings w ere 1, 500 feet. Middle and high clouds, layered to 25, 000 feet with bases at 10,000 feet, were also present over the southern area throughout the day.
Winds were east to southeasterly at 5-15 knots, becoming north to northeasterly of 10-20 knots in the afternoon and diminishing to 3-10 knots after sunset. "
Morning visibilities were near zero in dense fog throughout the area. The northern section cleared by 1200Z. Visibilities in the south rose to 3,200 meters at midday, then returned to as low as 800 meters for the rest of the day. Visibilities in the northern section were as low as 1,600 meters after sunset.
Temperatures fell in response to northerly winds. Highs were 10-18 degrees C; lows, 0-10 degrees C.
The Czechoslovak chemical detection team detected the nerve agent Sarin (GB) in two separate locations during the morning hours. In addition, Yperite (111)) was also detected. As noted above, the frontal patterns during this period moved to the south-southeast
20 January 1991
A weakening low-pressure area moved southeastward down the Persian Gulf to the Strait of Hormuz. Cool moist low-level air moved southwest and west over the Northeastern half of Saudi Arabia and extreme southwestern Iraq. Mid-level disturbances across the subtropical jet stream resulted in extensive middle and high cloudiness over northern Saudi Arabia and southern Iraq. By days end another low had crossed Syria toward western Iraq.
A 0000Z broken low clouds at 1,500-4,000 feet covered Baghdad and the Tigris-Euphrates river valley. These clouds slowly cleared from the northwest; by 2100Z, only broken middle and high clouds from 10,000 to 30,000 feet covered the southern half of the Valley. The northern half (including Baghdad saw only thin high clouds. Broken clouds were layered from 1,500 through 25,000 feet over the western slopes of the Zagros Mountains. Over the southern Zagros, tops reached 30, 000 feet. Isolated afternoon and evening thunderstorms reached 35.000 feet in the extreme southeast near the Zagros Mountains. After 2100Z, patchy broken low clouds formed again over the northern part of the Tigris Valley and the immediate Baghdad area; bases were 1,000 to 1,5000 feet; tops, 3,000 feet.
Light rain or showers fell over the southern half of the Tigris-Euphrates river valley and southwestern Iraq. There were isolated afternoon and evening thundershowers over the extreme southeast. Intermittent drizzle fell in the cool air moving west away from the northern Persian Gulf.
Winds were northwesterly to northerly over the Baghdad area, becoming northeasterly over the southern Tigris-Euphrates river valley. Over Kuwait and extreme southern Iraq, winds were northeasterly to easterly. Speeds diminished from 10-15 knots in the morning to 5-10 knots by mid-evening.
Visibilities in southern and southwestern Iraq and in extreme northeastern Saudi Arabia were near zero in fog during the night, but as high as 2, 000 meters in southern Iraq and Kuwait during mid-afternoon. After dark, they dropped rapidly to less than 500 meters. Visibilities in the Tigris-Euphrates river valley, northwest of the low clouds, improved to 10 km by late morning. Patchy dense river fog formed after 2100Z dropping visibilities to less than 500 meters.
High temperatures were 7-10 degrees Centigrade in the north and 18 degrees Centigrade in the south. There were freezing temperatures in Iraq and northern Saudi Arabia and subfreezing temperatures above 6,000 feet in the mountains of southeastern Turkey and northeastern Iraq. Central Saudi Arabian lows were 5-12 degrees C.
21 January 1991
Mid-level disturbances continued to move east-northeastern ward along the subtropical jet stream, crossing northern Saudi Arabia and Kuwait into Iran.
Patchy dense fog and low clouds again plagued southwestern Iraq and extreme northeastern Saudi Arabia until they dissipated in late morning. Cloud bases were from zero to 1,000 feet; visibilities, from near zero to 500 meters. Layered middle and high clouds persisted from 10,000 to 32,000 feet over most of northern and central Saudi Arabia and the central Red Sea
Extensive fog and low clouds also prevailed in this area. Cloud bases were from near zero to 500 meters, and lops reached 2,000 feet. The clouds and fog slowly dissipated by late morning over southwestern Iraq and northeastern Saudi Arabia as far east as Rafha and King Khalid Military City. Over northeastern Saudi Arabia, the low clouds and fog became broken with bases near 3, 000 feet and tops at 6, 000 feet by early afternoon. On the Saudi Arabian and Persian Gulf coast, early morning ceilings were also near zero, but by late morning, most clouds had become scattered. Patchy fog and low clouds reformed throughout all of northeastern Saudi Arabia and extreme southwestern Iraq shortly after dark Ceilings dropped to 200-500 feet by 2100Z. Layered middle and high clouds from 10,000-32,000 feet moved slowly southeastward over southern Iraq, northwestern Saudi Arabia and Kuwait; by 2100Z, they were over central and northeastern Saudi Arabia just southeast of Kuwait. Infrared satellite imagery taken just before sunrise in Kuwait shows these layered decks.
Precipitation, outside of thunderstorms and showers, was limited to light drizzle in areas of dense fog and low clouds.
Winds were northwesterly at 5-10 knots in southeastern Iraq and northeastern Saudi Arabia; they slowly became southeasterly at 5-10 knots in southwestern Iraq and in north-central and northwestern Saudi Arabia
Early morning visibilities in the fog and low cloud area ranged from zero to 500 meters, improving to 1,000-3,000 meters by late morning and to 5-5 kin by late afternoon. Visibilities were as low as 100 meters in desert fog patches. Patchy dense fog again formed after dark. The thickset fog was found along the Persian Gulf coastline and in shallow depressions inland where sand was still moist or where showers had occurred earlier in the day. On the Persian Gulf coast, visibilities improved from near zero at dawn to 1,000-2,000 meters by 0900Z, but dropped below 500 meters in fog by 1900Z. Patchy dense fog over and near the Tigris and Euphrates Rivers northwest of Basrah dissipated by 0600Z, but reformed after 1900Z.
22 January 1991
Easterly to east-northeasterly low-level winds continued to bring moisture to west-central and northwest Saudi Arabia. The sub tropical jet stream slowly weakened, but it continued to bring middle ad high clouds northeastward across the Arabian peninsula into Kuwait and southwestern Iran.
Multilayered broken middle and high clouds persisted over southwestern lraq, the southern Persian Gulf, and central Saudi Arabia from 10, 000 to 28,000 feet, Visibilities remained good except where mountains were obscured by cloud.
Fog and low clouds again persisted all night over northeastern Saudi Arabia the northern Saudi Arabian Persian Gulf coast, and extreme southwestern Iraq. Ceilings were again from near zero to 500 feet. Low clouds slowly lifted and dissipated, moving to a small area southwest of Kuwait by late morning. Bases were now 3,000 feet, with tops to 7,000 feet. Isolated thunderstorms, with bases as low as 2,000 feet, formed in late morning and early afternoon in extreme northeastern Saudi Arabia Kuwait, the northern Persian Gulf, and southwestern Iraq. Tops reached 40,000 feet. Layered broken middle and high clouds persisted from 10,000 to 27,000 feet throughout the day over central and northeastern Saudi Arabia Kuwait, and extreme southwestern Iraq. Iraq northwest of Basrah was clear. A visual DMSP satellite image taken shortly after sunrise in Kuwait, shows layered clouds with embedded thunderstorms over northeastern Saudi Arabia, the Persian Gulf, and southwestern Iron.
By sunset, low clouds and fog began to reform along the Iraq-Saudi Arabia border northwest as far as Rafha. By late evening, the fog had lifted into broken low clouds with bases from 1,000 to 2,000 feet and tops to 5,000 feet. These clouds had spread north and Northeastern as far as the central Tigris-Euphrates river valley by 2100Z.
Showers and thunderstorms fell over northeastern Saudi Arabia, Kuwait, the northern Persian Gulf, and southwestern Iran. Patchy nighttime drizzle fell in area of dense fog and low clouds.
Winds were northeasterly at 5 knots, becoming southeasterly at 5-10 knots after 0900Z.
Visibilities dropped to less than 100 meters in fog before dawn.
23 January 1991
By mid-afternoon, the frontal system had moved south of Baghdad. A weak high pressure center formed over Kuwait early in the day and moved slowly southeast in the northern Persian Gulf.The weak stationary frontal system in central Saudi Arabia weakened further. The southwest to northeast subtropical jet stream over central Saudi Arabia moved southeastward to Qatar by 2100Z.
Isolated blowing dust reduced visibilities to as low as 3,200 meters in western Iraq.
Extensive broken to overcast low clouds, with bases of 500-1,000 feet and tops to 1,500-2000 feet, covered northeastern and central Saudi Arabia. By early afternoon, skies were scattered to broken and bases had lifted to 3, 000 feet. This laser dissipated shortly before sunset over northeastern Saudi Arabia, but reformed by 2000Z. In early evening, broken low clouds from 3,000 to 5,000 feet moved north and northeastern ward over Kuwait and the southern Tiger-Euphrates river valley in advance of the southward-moving cold front. By 1200Z, the leading edge of broken to overcast frontal cloud lasers had moved south of Baghdad, with bases from 3,000 to 4,000 feet: lops were 12,000-15,000 feet with broken high clouds above. Isolated rain showers along and just ahead of the front reached 20,000 feet. By 2000Z, the leading edge of the frontal clouds had moved to near An Najaf in the Tigris-Euphrates river valley --the trailing edge was 60 miles north of Baghdad. Figure 3-8, a visual satellite image taken at 1037Z, shows these layered clouds well.
Isolated moderate to heavy rain showers fell in central Iraq along and within 100 miles either side of the southeastward-moving cold front. Patchy light drizzle fell in northeastern Saudi Arabia before 0500Z.
Winds were easterly at 5-7 knots before dawn, becoming southeasterly at 5-10 knots by late morning in extreme southern Iraq and northeastern Saudi Arabia. By 1700Z winds had veered to southerly at 10-15 knots. In central Iraq, winds were light and variable until 1200Z, becoming southerly at 10-20 knots after 1500Z.
24 January 1991
A 1200Z, heavy rain fell in extreme northern Saudi Arabia near the western Iraq border Fog formed during the night and through the morning in northern Saudi Arabia, along the western Saudi Arabia-Iraqi border, in northern Jordan, and in southern Syria
Winds were westerly to northwesterly at 10 knots during the first 12 hours, becoming northerly to northeasterly at 10 knots later in the day.
Visibilities in fog were as low as 5 km from 0000 to 1000Z in Saudi Arabia
25 January 1991
A low moved east-northeast across Syria and Iraq, producing light snow and rain showers, blowing dust, and extensive cloudiness. Conditions improved toward the end of the day as the system moved into Iran. By the end of the day, another low had developed along the eastern Mediterranean coast, increasing cloudiness in western Iraq.
The low produced light snow over western Iraq, northeastern Jordan, and Syria; light rain showers fell in northwestern Saudi Arabia and Iraq. Winds to 20 knots in northern Saudi Arabia produced duststorms from 0900 to 1500Z as far south as 28 degrees north.
Cloud cover was extensive until evening, by which time the system had moved into Iran. Broken to overcast low and middle clouds, along with some high clouds, preceded the low and its cold front. Scattered to broken low clouds followed the front; ceilings were 2,000-3,000 feet, but as low as 500 feet in rainshowers.
Precipitation consisted of light rainshowers that developed with the frontal system. At Z, Baghdad skies were overcast with rainshowers.
From 0400 to 1100Z in Saudi Arabia, fog reduced visibility to as low as 3,600 meters. Fog redeveloped in the evening. Some dust may have been advected into the area from storms farther west.
26 January 1991
By 1800Z, a weak secondary low had formed along the front in Saudi Arabia near 27 degrees North, 44 degrees East, and drifted slowly east.
The low-pressure system produced light snow over southern Syria and light rainshowers in northern Saudi Arabia and western Iraq. Blowing dust south of the rain in Saudi Arabia reduced visibilities to 5 km. Winds were 20 knots around the low, but reached 30 knots with rain in northwestern Saudi Arabia
The low moving across southern Iraq produced extensive cloudiness, as well as thunderstorms with bases at 2, 000 feet and tops to 35,000 feet. Ceilings were as low as 800 feet in rainshowers.
Precipitation fell as light rain ad rainshowers in Saudi Arabia around the low. Rainshowers also fell in Iraq.
Winds were northwesterly at 5-15 knots most of the day, becoming northeasterly as the storm system approached and northwesterly again as it passed. Peak speeds were 23 knots, probably higher in Iraq.
Visibilities in eastern Iraq were 6 km in haze early in the day through 0600Z. Later in the day, visibilities on the south sides of showers and duststorms were reduced to 8 km.
27 January 1991
A low moving eastward from northeastern Saudi Arabia to the Persian Gulf coast produced extensive cloudiness over most of southeastern Iraq. The low gradually weakened throughout the day leaving only some low clouds in the vicinity of the Gulf by late evening. A cold front extended west-southwest from the low across Saudi Arabia. A strong high moved into northwestern Saudi Arabia, driving the cold front into southern Saudi Arabia; strong winds behind the front produced dust storms.
The storm system produced significant weather over large parts of Saudi Arabia. Light rain and rainshowers moving east with the low persisted at some Gulf coastal stations until 1900Z. The low produced mutilayered clouds the first half of the day, but only low clouds the second half. A low overcast with fog developed behind the front in northwestern Saudi Arabia; fog dropped visibilities to as low as 200 meters. Skies improved by mid-morning and cleared by afternoon. Strong winds behind the front produced dust storms. Visibilities in northwestern Saudi Arabia were near zero in early evening because of blowing dust in 35 knot winds.
Skies were initially overcast in the southeastern two-thirds of the area but Baghdad and vicinity was clear. Middle and high clouds were only present the first half of the day; they dissipated and moved off to the east by 1200Z. The low clouds moved southeast during the day and were out of Iraq by 1500Z. After 1500Z, the low cloud remaining over Saudi Arabia and Kuwait was broken to overcast.
Precipitation fell from 0000 to 0600Z as light drizzle, rain, and rain showers.
Winds were initially southeasterly at 10-15 knots ahead of the low, by northerly to northwesterly across Iraq behind the front. Winds shifted across the area by 120OZ; northerly to northwesterly winds were 10-20 knots with peak gusts to 30 knots. Speeds dropped to less than 10 knots during the evening.
Visibilities dropped to 9 km under the cloud cover in rain, fog, and haze.
28 January 1991
High pressure began to dominate the weather over Iraq and northern Saudi Arabia, but parts of Saudi Arabia were still affected by weather left in the wake of the low-pressure system that prevailed on the 27th.
Morning fog and low clouds north of Riyadh lowered ceilings and visibility to 2,000 feet and 8 km. There were some scattered to broken low clouds in the western Persian Gulf and at coastal stations. There was broken fog and stratus, with blowing dust, in southern Saudi Arabia.
Skies were generally clear except for thin scattered high cloud at 22,000-28,000 feet over northern Iraq and heavy black smoke over southern Iraq--see Figure 3-14. Winds were northwesterly at 3-10 knots, becoming more northerly toward the end of the day. Visibilities were as low as 1,500 meters over southern Iraq in the heavy smoke.
Visible Smoke Plumes
NOAA visual imagery in Gulf War Weather shows smoke plumes visible originating in an area just south of the two large lakes west of Baghdad and extending to the southeast. Available NOAA thermal imagery details smoke plumes in eastern Iraq moving to the southeast.
29 January 1991
A high-pressure area over Saudi Arabia weakened as it moved southeast toward Qatar. A mid- to upper-level disturbance moved across the northern part of the region, resulting in extensive cloudiness over northern Iraq and Turkey.
The disturbance produced light min and snow in Syria and snow in Turkey. There was extensive black smoke along the Persian Gulf coast. Suspended dust still reduced visibility in southern Saudi Arabia.
Isolated evening thunderstorms from 3, 000 to 35, 000 feet developed over southeastern Iraq. Some formed southwest of Baghdad at 1800Z.
Winds were near calm during the night, becoming east southeasterly at 5-10 knots in the morning and increasing 10-20 knots during the afternoon. On the Persian Gulf- coast, however, winds were northwesterly at 5-10 knots for the first half of the day before switching to east-southeast.
Visibilities were 8 km in blowing dust in the afternoon as the winds picked up. Black smoke reduced visibilities along the Persian Gulf coast--one station reported 9 km.
30 January 1991
A low-pressure system developed in the eastern Mediterranean and moved eastward across Syria, reaching western Iraq by the end of the day.
Low clouds moved into western Iraq during the day with ceilings around 3,000 feet. The subtropical jet stream produced high clouds across central Saudi Arabia.
Cloud cover from the previous day 's disturbance remained over eastern Iraq and Kuwait; broken low clouds at 3,000-6, 000 feet in the north around Baghdad dissipated by 1100Z. Over Kuwait, broken middle clouds from 8,000 to 14,000 feet moved off to the east by 0600Z. Broken to overcast low clouds with 3,000-foot ceilings and 6,000-foot tops entered the western part of the area in the evening.
With the storm system approaching, winds were southerly to southeasterly at 5-10 knots.
Visibilities were restricted, primarily by haze and smoke from burning oil. Morning fog reduced visibility to 5 km in some spots; most haze restrictions were reported at 8km. Some dust was raised during the day with increasing winds from the approaching system.
Visible Smoke Plumes
DMSP visual imagery in Gulf War Weather shows smoke plumes originating in an area west of the two large lakes west of Baghdad and extending to the southeast. The plume splits into two plumes, one extending to the east and the other to the SSE just south of the southernmost lake.
31 January 1991
A slow-moving low in the eastern Mediterranean Sea spread stormy weather throughout the Middle East as an associated frontal system passed through Iraq. At 0600Z, a secondary low-pressure cell was centered southwest of Baghdad. It rapidly moved northeastern while the cold front moved south and weakened. In north-central Saudi Arabia the strong subtropical jet stream spread extensive high clouds.
Broken to overcast low clouds extended over the area until about 1600Z, with ceilings over Iraq as low as 3, 000 feet and tops to 6, 000 feet. Baghdad was affected between 0200 mid 0900Z. Skies become clear in central Iraq and Kuwait after 1600Z as the front moved southward.
Isolated thunderstorms with tops to 35, 000 feet passed northeast of Baghdad near 1100Z. Rain fell in western Iraq when the low-pressure cell moved through.
Winds were southwesterly at 5-10 knots before the front and westerly to northerly at 15-20 knots immediately behind it.
Visibilities were reduced to 4,000 meters by duststorms in Kuwait and southern Iraq as the front passed. Ground fog lowered visibilities to about 6 kin in northeastern Saudi Arabia, Kuwait, and southern Iraq.
1 February 1991
High pressure was centered over northwestern Saudi Arabia, keeping central Iraq cloud-free. A weak cold front extended from a low centered in north central Iran. The front spread middle clouds from Qatar southwestward across Saudi Arabia. A slow-moving low-pressure system centered on the Turkey-Syria border caused rainshowers in western Iraq, Syria, and Jordan. By 1800Z, middle clouds from this low reached Baghdad. A weak low developed on the central Red Sea coast in response to an upper-air disturbance.
Middle clouds covered the mountains to Iraqs west and north. Light rain fell in Syria and northern Iraq between 1800 and 2100Z. Extensive areas of mountain-wave turbulence developed in the west between 0300Z and 1500Z and reached at Far East as 43 degrees east. Early-morning ground fog formed in low-lying areas over most of the eastern Arabian Peninsula. Lowest visibilities were 2,000-4,000 meters.
Skies were clear to scattered before about 0900Z, except in the extreme northeast. Broken low clouds from the low in Turkey spread southward; by 1600Z, they had reached Baghdad, with 3,000 foot ceilings. Thin broken or scattered cirrus spread northeastward from the northern Red Sea, covering the area south of 31 degrees North by 1100Z.
Winds were northeasterly at 5-10 knots in the south, westerly to the north. Afternoon winds were light and variable over central Iraq. Visibilities were generally good, but morning ground fog reduced them to about 6 km in northeast Saudi Arabia, Kuwait and southern Iraq.
2 February 1991
A trough of low pressure formed to the east of a high-pressure cell centered over eastern Saudi Arabia, causing low clouds in southern Iraq. A frontal system with low centers in the southern Caspian Sea and in east central Syria extended along the northern Iraq border. The strong subtropical jet stream spread high and middle clouds over central Saudi Arabia.
Low and middle clouds prevailed over northern and western Iraq. Early morning ground fog formed in low-lying areas over most of the Eastern Arabian Peninsula. Extensive areas of mountain-wave turbulence developed near the Syria-Iraq border between 0300 and 1500Z and reached to 43 degrees East.
The subtropical jet stream caused layered middle and high clouds over the area south of 32 degrees North throughout the day. Ceilings were between 15,000 and 25,000 feet, with the lowest along the northern Persian Gulf. Frontal low clouds stretched along the Syria-Iraq border The broken low clouds southwest of Baghdad included 4,000 foot ceilings and 6,000 foot tops. These clouds gradually moved east; by 2000Z, they were on the Kuwait coast. Another layer of low clouds with ceilings of about 3, 000 feet formed over the Tigris-Euphrates river valley north of 31 degrees North during the night.
Winds were easterly at 10-15 knots south of 30 degrees North, southerly in the central area and westerly north of 33 degrees North. They were gusty in the southern areas.
Duststorms reduced visibilities in the northern Nafud Desert eastward to Southern Kuwait between 1200 and 2000Z. Minimum visibility was about 2,400 meters. Dense smoke was reported in Northwestern Kuwait before 0800Z--visibiliies were probably below 2,000 meters.
High temperatures were 13-16 degrees Celsius; lows, 2-11 degrees Celsius.
3 February 1991
The frontal system in eastern Syria began to move slowly eastward and break up, resulting in lowered ceilings and gusty winds. The nearly dry front passed Baghdad at 2000Z. A weak front extended from central Iraq to near Riyadh, spreading low clouds to Iraq's eastern section. The subtropical jet stream became more westerly than northwesterly, leaving the northern Persian Gulf cloud-free but spreading scattered to broken middle and high clouds across Saudi Arabia.
Sustained winds to 25 knots were reported in extreme northwestern Saudi Arabia as the front passed. Extensive duststorms reduced visibilities to 1,000 meters near the front in the Syrian and Nafud Deserts. Duststorms were also reported at 1500Z between Riyadh and Kuwait.
Middle and high clouds from the subtropical jet stream had moved out of the area by 1000Z. In the morning, scattered to broken low clouds covered Iraq east of 43 degrees East and all of Kuwait. Some locations reported 3,000 foot ceilings. By 1200Z, the clouds had moved eastward to the Iraq-Turkey border. A small area of low clouds with 3,000 foot ceilings formed about 100 miles west of Baghdad at 1600Z.
Winds were westerly at 10-25 knots west of 45 degrees East, but southeasterly at 10-15 knots to the east. There were gusts to 35 knots near the front.
Duststorms reduced visibilities to as low as 500 meters at about 1500Z in southern Kuwait and northeastern Saudi Arabia. Elsewhere, visibilities were above 6 km. High temperatures were 8-20 degrees Celsius; lows, 3-16 degrees Celsius.
4 February 1991
High pressure centered in southeastern Egypt strengthened and built into northwestern Saudi Arabia. The low -pressure system that had been affecting northern Iraq continued to move eastward. By 0900Z, the trough had moved southeastward to the south of Qatar. The subtropical jet stream continued to spread high and middle clouds over the central Arabian Peninsula.
In the early morning, middle clouds produced 10,000 foot ceilings in a triangular area between 30 degrees North and a southwest-Northeastern line running from 60 miles south of Baghdad, then eastward to the Iraq border. These clouds rapidly moved southeastward. By 0600Z, they affected only the coast of Kuwait. The area was almost cloud-free by I000Z.
Winds were northeasterly at 10-15 knots inland, but northerly at 15-20 knots on the Kuwait coast. Inland, winds became northerly at 5-10 knots after 1800Z.
Visibilities were generally above 10 km, but scattered fires and smoke plumes reduced visibility in Kuwait to below 4 km. One smoke plume, originating in southern Kuwait measured, 35 miles long and 10-15 miles wide.
High temperatures were 3-13 degrees Celsius; lows, 2-8 degrees Celsius.
5 February 1991
High pressure centered in central Iraq kept skies clear or scattered most of the day, but clouds associated with the subtropical jet stream still spread high and middle clouds over the central Arabian Peninsula. These clouds were scattered in the morning, but denser clouds moved in from Egypt by 1000Z.
Morning haze reduced visibilities in central Saudi Arabia, Riyadh reported 4,800 meters at 0500Z, improving to 8 km by 0800Z. Duststorms after 2000Z were the result of 20-knot winds over the Syrian and Nafud Desert; they lowered visibility to 5 km.
Clouds were limited to scattered cirrus until about 1100Z, but the subtropical jet strewn moved scattered to broken middle and high clouds into southwestern Iraq later in the day. These clouds had moved over Kuwait by 1600Z, producing 10,000-foot ceilings during the night.
Winds were northeasterly at 10-15 knots along the coast, but light and variable in Iraq. As the front shifted farther north after 0900Z, winds in the south became stronger and more easterly. Visibilities were above 10 km except in Kuwait, where scattered fires and smoke plumes reduced visibility to below 4 km. High temperatures were 9-17 degrees Celsius; lows, 0-6 degrees Celsius.
Visible Smoke Plumes
DMSP visual imagery in Gulf War Weather shows small visible smoke plumes over Kuwait extending to the south and southeast.
6 February 1991
High pressure was centered in northwestern Iraq, with a weak low-pressure trough to the southeast between central Saudi Arabia- near Riyadh--and Israel. The subtropical jet stream remained over the northern Arabian Peninsula; associated high clouds became increasingly scattered after 0600Z.
At 0000Z, them were only scattered low, middle, and high clouds throughout the area. By 0300Z, the middle cloud deck had thickened, ceilings as low as 12,000 feet, with tops at about 18,000 feet, had formed over the southwestern half of Iraq. These clouds drifted eastward and by 1900Z they were east of Baghdad and Kuwait. Middle and high clouds from the subtropical jet stream affected Kuwait and southern Iraq between 0400 and 1100Z; bases were at or above 10,000 feet, with tops to 32,000 feet.
Winds were light and variable in Iraq, but easterly at 5-10 knots in Kuwait. Morning fog, smoke, and dust reduced visibilities in Kuwait and southern Iraq to as low as 3,200 meters in spots. Afternoon visibilities in areas not affected by smoke were above 6 km.
Afternoon high temperatures were between 5 and 13 degrees Celsius. High pressure and almost clear skies drove morning low temperatures down to -2 degrees Celsius in the north and 7 degrees Celsius in the south.
7 February 1991
A low-pressure system over northeastern Saudi Arabia resulted in afternoon and evening rainshowers and thunderstorms over Saudi Arabia and the Persian Gulf. The subtropical jet stream brought middle and upper cloudiness to central Saudi Arabia Weak high pressure was centered over Iraq.
Scattered low clouds, with some middle and high clouds that were occasionally broken, extended across central Saudi Arabia and the Persian Gulf. Ceilings varied from 10,000 to 25,000 feet. Broken low clouds with bases at 2,000feet were evident early in the morning over western Iraq. Light afternoon rainshowers fell over east central Saudi Arabia. Isolated late evening thunderstorms were reported over the west-central pan of the Persian Gulf. Tops were about 30,000-35, 000 feet. Visibilities in northwestern Saudi Arabia were 7-9 kin in haze and suspended dust. Suspended dust also reduced early morning visibilities in east central Saudi Arabia to 4,800 meters.
Early morning skies were generally clear, but scattered middle clouds from the west moved into central Iraq and Kuwait by mid-morning. The middle clouds over central Iraq went scattered to broken at 10,000 feet by late morning. Skies became scattered by early afternoon. By early evening, cloud cover over Kuwait and southeast Iraq became scattered, variable to broken, at 10,000-18,000 feet. Isolated evening thunderstorms developed over extreme northern Kuwait; tops reached 30,000 feet.
Early morning winds were light and variable, becoming northwesterly to northerly at 10-15 knots by late morning. Haze and suspended dust reduced visibilities over central Iraq to 7-9 km. Smoke, haze, and suspended dust reduced visibilities in northern Kuwait to 5-7 km and to 1,600 meters in southern Kuwait.
High temperatures were 7-15 degrees Celsius; los, 0-6 degrees Celsius.
Visible Smoke Plumes
NOAA visual imagery in Gulf War Weather shows visible smoke plumes extending in varying directions from to the northeast to the south. Imagery captioned: "Smoke from Kuwait is being blown southward into northeastern Saudi Arabia. [13]
8 February 1991
The low pressure system was now located over southeastern Saudi Arabia. The subtropical jet stream brought middle and high clouds across eastern Saudi Arabia. Weak high pressure was centered over Iraq.
Although skies w ere generally clear, broken middle clouds at 10, 000 to 12,000 feet were observed over east-southeastern Saudi Arabia during early morning. Skies were broken to overcast at 4,000-5,000 feet between 0500 and 1300Z over northwestern and north-central Saudi Arabia. Scattered middle clouds were observed over western Iraq in the morning and afternoon, becoming broken at 10,000-12,000 feet duping the evening. Blowing sand and dust lowered visibilities to 5-7 kin in east central Saudi Arabia.
Skies were generally clear, but scattered middle clouds were observed over southeastern Iraq duping early morning. By mid-afternoon, there were scattered middle clouds over central Iraq. By late night, these became scattered to broken at 10,000-12,000feet.
Winds were light and variable in the morning, becoming northwesterly to northerly at 10-15 knots. Visibilities in smoke over southern Kuwait and southeast Iraq were less than 1,600 meters . High temperatures were 7-15 degrees Celsius; lows. 0-6 degrees Celsius.
Visible Smoke Plumes
NOAA visual imagery in Gulf War Weather shows visible smoke plumes over southeast Iraq and southern Kuwait, extending to the south and southeast.
9 February 1991
High pressure dominated the region-- skies were generally clear.
Skies were clear except for scattered low clouds over northwestern Saudi Arabia and western Iraq. Winds increased to 15 knots with gusts of 25 knots across northern Saudi Arabia, where afternoon visibilities decreased to 4,800 meters in blowing sand and dust.
Early morning skies over central Iraq were broken at 10, 000-12,000 feet. The clouds slowly moved into southeastern Iraq and dissipated during the day.
Winds were westerly to northwesterly at 10-20 knots. Smoke and haze lowered visibilities in Kuwait to 5-7 km. High temperatures were 12-20 degrees Celsius: lows. 2-8 degrees Celsius.
10 February 1991
High pressure continued to dominate. Skies over Saudi Arabia and Iraq were clear during the day, but scattered to broken mid-level clouds with bases at 10,000-12,000 feet moved into western Iraq by late evening.
Skies were clear during the day, but by late evening, scattered to broken mid-level clouds with bases at 10,000-12,000 feet moved into central Iraq.
Winds were northwesterly at 5-10 knots. Thick smoke over east and southeast Iraq began to show in satellite photos by 0600Z and lasted until early evening. Smoke from southern Kuwait was also still visible; visibilities in the smoke were 800-1,600 meters. High temperatures were 10-15 degrees Celsius; lows, 0-5 degrees Celsius.
Visible Smoke Plumes
Imagery in Gulf War Weather shows smoke plumes visible over western, eastern, and southeastern Iraq. Direction: SSE; Smoke plumes are also visible over southern Kuwait. Direction: South.
11 February 1991
High pressure was centered over southeastern Saudi Arabia but low pressure formed over western Saudi Arabia. The subtropical jet stream brought increased moisture in the mid- and upper-levels to Iraq and northern Saudi Arabia. A mid-level disturbance moving over Iraq and northern Saudi Arabia caused isolated thunderstorms and rainshowers.
Scattered high clouds over western Iraq became broken with bases at 20,000 feel from mid-morning through afternoon. There were scattered low clouds over northwestern and east central Saudi Arabia during the day.
Scattered to broken upper clouds with bases at 22,000 - 25,000 feet were present during the morning and mid-afternoon over central Iraq. Morning skies were clear over Kuwait and southeastern Iraq, but smoke plumes were visible. Cloudiness decreased in central Iraq during the day, but increased in southeastern Iraq and Kuwait. Skies became scattered to broken, occasionally overcast, at 4,000 - 6,000 feet. By late afternoon, thunderstorms (tops 35,000feet) and rainshowers had formed over Kuwait; they moved off to the east and dissipated by late evening.
Winds accompanying the thunderstorms in Kuwait reached 25-35 knots, but over the rest of the area they were northwesterly at 10-15 knots.
Smoke and haze lowered morning visibilities to 4,800 meters in Kuwait and southeastern Iraq. Rain and rainshowers reduced evening visibilities to 1,600 - 3,200 meters. High temperatures were 10-15 degrees Celsius; lows were 0-5 degrees Celsius.
Visible Smoke Plumes
Imagery in Gulf War Weather shows smoke plumes clearly visible over Kuwait. Direction: South; Smoke plumes are also visible over southeastern Iraq. Direction: SSE.
12 February 1991
High pressure dominated, but a low-pressure system moved into the eastern Mediterranean by the end of the day increasing cloudiness over western Iraq.
Broken middle clouds at 8,000-10,000 feet were present over northeast, east and central Saudi Arabia and the Persian Gulf during the morning. By late evening, them were scattered to broken high clouds at 20,000-25,000 feet over western Iraq.
Broken middle clouds at 8,000-10,000 feet remained over Kuwait until mid-morning. Scattered upper clouds moved into central Iraq by late evening.
Winds were northwesterly, to northerly at 10-15 knots. High temperatures were 10-15 degrees Celsius; lows 0-5 degrees Celsius. Visibilities in Kuwait were 5-7 km due to smoke and haze
Visible Smoke Plumes
Imagery in Gulf War Weather shows smoke plumes clearly visible over eastern Iraq and Kuwait. Direction: S-SSE.
13 February 1991
High pressure dominated the Saudi Arabian peninsula but low pressure centered over the eastern Mediterranean sent moisture into Iraq and northern Saudi Arabia. The low moved to the northeast as high pressure intensified behind it.
Scattered skies became broken to overcast over western and northern Iraq. The 25,000 foot ceilings prevailing in the morning became 8,000- 10,000 feet during the day. By the end of the day, skies were scattered again. Over northern Saudi Arabia, skies were scattered, but occasionally broken, at 20,000-25, 000 feet.
Scattered skies became gradually broken over central, east-central, and southeast Iraq and Kuwait. Smoke plumes were visible over southern Kuwait and the northern Saudi Arabian Gulf Coast. (see below)
Winds were northwesterly at 10-15 knots. Visibilities in southeastern Iraq and Kuwait were 5-7 kilometers in smoke and haze. High temperatures were 13-16 degrees Celsius; lows, 1-4 degrees Celsius.
Visible Smoke Plumes
Imagery in Gulf War Weather shows smoke plumes clearly visible over southern Kuwait. Plume directions appear to be to the S-SSE.
14 February 1991
High pressure over Iran and Syria resulted in fair weather across most of the region.
Morning skies over northern Iraq were overcast with middle and high clouds; ceilings were as low as 10,000 feet. The clouds moved eastward and were over Iran by 1200Z. Broken low and middle clouds over central and southern Saudi Arabia produced 5,000foot ceilings with scattered light rainshowers and 9-km visibilities. The clouds moved southeastward and became scattered after 1200Z. Visibilities in western and southern Mail were as low as 6 km where 20-knot winds resulted in localized suspended and blowing dust.
Cloud cover consisted only of thin scattered high clouds over eastern Iraq and Kuwait: bases were 20,000 feet; tops 25,000 feet. The high clouds moved east into Iran by 1200Z. Winds were light and variable in the early morning, becoming northerly to easterly at 5-15 knots during the day.
Morning visibilities along the Persian Gulf coast near Kuwait were 8 km in fog. Widespread haze over northern Saudi Arabia produced visibilities of 8 km. High temperatures were 16-18 degrees Celsius; lows were 2-5 degrees Celsius.
Visible Smoke Plumes
Imagery in Gulf War Weather shows smoke plumes clearly visible over southern Iraq. Plume directions appear to be to the SE.
15 February 1991
High pressure over Iran and Turkey extended southward across most of the region. Broken high clouds passed through western Iraq to the east during the afternoon, followed in the evening by a large shield of high cloud entering from the west. Scattered to broken high clouds over parts of central and southern Saudi Arabia-with bases between 9,000 and 12,000 feet--dissipatedparrially during the day. Blowing dust in northern and western Saudi Arabia reduced visibilities to as low as 5 km.
Broken high clouds passed through the area between 130OZ and 2100Z with bases at 24,000 feet and tops to 32,000 feet. There were followed by scattered high clouds that moved into central Iraq from the west by the end of the day. Scattered bases were at 24,000 feet with tops to 32,000 feet.
Winds were northerly at 5-10 knots through the morning, gradually shifting to easterly of 5-15 knots in the afternoon and evening. Smoke that is clearly visible restricted visibility up to 14,000feet. Evening ground fog developed along the Kuwait coast, dropping visibility to 8 km. High temperatures were near 20 degrees Celsius; lows varied from 2 degrees Celsius in the north to 8 degrees Celsius in the southeast.
Visible Smoke Plumes
DMSP visual imagery in Gulf War Weather shows smoke plumes visible over Kuwait extending to the south over Saudi Arabia.
16 February 1991
High pressure over Iran weakened as a strong frontal system approached from the west. The polar jet stream dipped southward into the eastern Mediterranean as the subtropical jet stream crossed Egypt and brought in upper-level moisture. A new low-pressure center formed on the front over Syria by 1500Z and moved southeast. The low and its accompanying cold front reached western Iraq by 1800Z.
Multiple cloud lasers covered the region southward to 25 degrees North with scattered to broken low clouds and broken to overcast middle and high clouds. Light rain and rainshowers lowered ceilings to 1,000 feet and visibilities to 1,100 meters. The blowing dust already present in northwestern Saudi Arabia at 0000Z spread to include much of northern Saudi Arabic, especially south of the rain. Winds up to 30 knots produced dust storms with visibilities as low as 200 meters in northern Saudi Arabia, Syria and western Iraq.
Cloud cover increased and ceilings lowered during the day. Skies were initially scattered with high clouds from 27,000 to 30,000 feet, but became broken to overcast by morning, with multiple lasers between 25,000 and 35,000 feet. Bases lowered to 20,000 feet by 0700Z. Broken middle clouds reached central Iraq at about 1100Z with 12,000 foot bases and 18,000foot tops. Scattered low clouds moved in by early evening with 2,000 foot bases and 6,000 foot tops; middle-cloud ceilings were down to 8,000 feet by then. Low clouds increased in the evening. Light rain and rain showers lowered ceilings to 1, 000 feet.
Winds varied from easterly to southerly with the approaching frontal system. Initial 5- to 10-knot speeds increased during the day. The highest reported sustained speed was 30 knots.
Visibilities worsened throughout the day. Dense black smoke over the southern half of Kuwait reduced visibilities to 6 km-- some pilots reported certain areas as "unworkable." Duststorms developed at wind speeds reached 20 knots around 0900Z; speeds to 30 knots dropped visibilities to as low as 200 meters later in the day. Local evening visibilities were as low as 1,100 meters. High temperatures increased to 20-25 degrees Celsius as the front brought warm air into the region; lows were 6-8 degrees Celsius.
17 February 1991
A low-pressure area moved northeast from central Iraq across Iran as its cold front moved through most of Iraq. A weak secondary low formed along the front in south-central Iraq near the Saudi Arabian border. The cold front continued southward into central Saudi Arabia and weakened. High pressure intensified behind the front.
Rain fell along the front in northern Saudi Arabia early in the day, but moved into central Saudi Arabia by evening. Visibilities were 8 km, but dropped to 4,700 meters in a 1500Z thunderstorm in west-central Saudi Arabia. Blowing dust ahead of the front reduced visibilities to as low as 1, 700 meters. Duststorms behind the front dropped visibility as low as 900 meters in western Iraq. Skies over central Saudi Arabia w ere scattered as 4, 000 feet, and broken to overcast at 10, 000 feet
Cloud cover from 0000Z to 1100Z was broken to overcast with layered low and middle clouds: ceilings were 3,000 feet, tops to 15,000 feet. Skies over southern Iraq and Kuwait were overcast at between 20,000 and 35,000feel. Skies in Iraq began to clear by 1100Z, leaving scattered low clouds from 3, 000 to 6,000 feet that continued moving east and south; all of Iraq, except for its extreme northern border, was clear after 1600Z.
Rain and rainshowers fell over northeastern Saudi Arabia southeastern Iraq, and Kuwait. The bases of late-morning thunderstorms near the Saudi Arabia border were 3,000 feet, with tops to 35,000 feet. The rain moved eastward by evening.
Winds were southerly to southeasterly at 5-15 knots ahead of the low and cold front, and northerly to northwesterly at 5-20 knots behind it. Speeds diminished to 5-10 knots in the evening.
Visibility in rain was 4,700 meters. Blowing dust in some areas of northeastern Saudi Arabia that had remained dry lowered visibilities to 6 km. Evening fog formed locally where rain had fallen, lowering visibilities to 6 km.
Daytime temperatures were highest (20 degrees Celsius) in the west where skies cleared first, but highs in the east were as low as 14 degrees Celsius. Daily lows were in the evening after the cold front had passed. Lows ranged from 6 degrees Celsius in the north to 12 degrees Celsius in the south.
18 February 1991
A high-pressure cell moved over Iraq and dominated much of the region weather. Morning fog developed over north-central and northwestern Saudi Arabia but dissipated by early afternoon. Clouds associated with yesterday's cold front were over central Saudi Arabia and the Persian Gulf, where they produced scattered light rain through the morning until moving into the Arabian Sea in the afternoon. Skies were scattered from 3,000 to 6,000 feet, broken from 10,000 to 18,000 feet, and broken from 28,000 to 33,000feet.
Thick morning ground fog lifted to form 1,000 foot ceilings that dissipated by about 1000Z. Broken middle clouds over southern Kuwait and northwestern Saudi Arabia moved off to the southeast during the first 6 hours of the day; ceilings were 7,000 feet with tops to 12,000 feet. Middle and high clouds moved into the region from the northwest during the second half of the day; scattered to broken middle clouds were from 8, 000 to 18,000 feet and thin broken high clouds were from 29, 000 to 35,000 feet.
Winds were generally light and variable in the north, but northerly to northeasterly at 5-10 knots in the south. Visibilities ranged from near zero to 2, 000 meters in thick and extensive morning fog across portions of Iraq and Saudi Arabia. The fog, which was concentrated over (and to the west of) the Tigris-Euphrates river valley in Iraq, didn't bum off until about 1000Z. Fog formed again in the evening over northern Saudi Arabia and Kuwait, dropping visibilities to 4,800 meters. High temperatures were 17-20 degrees Celsius; lows ranged from 5 degrees Celsius in clear areas to 11 degrees Celsius under the fog.
19 February 1991
A low-pressure area developed over Syria and moved eastward into northwestern Iraq. A, secondary low developed in northwestern Saudi Arabia and moved eastward into northern Saudi Arabia. Two lines of strong thunderstorms-- one over northern Saudi Arabia one over Iraq-- developed between 1500 and 1800Z and continued well into the next day.
Scattered low clouds over western Iraq and northern Saudi Arabia early in the day were from 3,000 to 5,000feet. Thin high clouds moved in that afternoon, Thunderstorm bases were at 3,000 feet, tops to 35,000 feet Rain and rainshowers began after 1500Z. In central Saudi Arabia, scattered to broken low and middle clouds, with bases at 4.000 and 10,000 feet, produced scattered evening rainshowers.
Cloud cover in the first 6 hours was limited to southeastern Iraq and Kuwait, where skies were scattered at 3,000 and 5,000 feet and thin broken from 20,000 to 25,000 feet. After these had cleared out in the afternoon, a new high thin broken layer at 22,000 to 25,000feet moved in. Convective actively from the west entered the area at about 1800Z, producing bases that were generally 3,000 feet, but as low as 1,000 feel in thunderstorms; tops were to 35,000feet Convective cells consolidated to form a nearly solid, north-south line in central Iraq as another, similar line formed in northern Saudi Arabia Middle-cloud ceilings outside showers were at 10,000 feet.
Thunderstorms produced localized moderate to heavy rain after 180OZ. Light rain and rainshowers fell outside the areas of strong convection.
Winds were east southeasterly at 5-10 knots during the first half of the day, increasing to 15-20 knots by afternoon. Isolated gusts to 30 knots occurred with thunderstorms. Visibilities were less than 1,000 meters in rain associated with thunderstorms, but 7 and 9 km elsewhere in rainshowers, black smoke from Kuwait, fog, and or blowing dust. High temperatures were 19-21 degrees Celsius; lows, 7-11 degrees Celsius.
Visible Smoke Plumes
DMSP visual imagery in Gulf War Weather shows smoke plumes visible over Kuwait and extreme northeastern Saudi Arabia.
20 February 1991
The low over Iraq moved eastward into Iran as the secondary low over northern Saudi Arabia moved southeast along the Persian Gulf coast. Thunderstorm activity that started the day before continued across eastern Iraq, Kuwait, and northeastern Saudi Arabia Lines of thunderstorms moved gradually eastward as new cells developed on their southwestern ends.
A cold front moved southeast across central and eastern Saudi Arabia, producing scattered rain showers and visibilities as low as 800 meters in blowing dust. Skies were scattered from 4,000 to 6,000 feet and broken from 10,000 to 15,000 feet. Thunderstorms that had been in northern Iraq earlier in the day moved into Iran, followed by broken to overcast low and middle clouds with ceilings at 3,500 feet. Western Iraq remained generally clear
Thunderstorms moved across the area from west to east. Bases were at 1,000 feet and tops reached 40,000 feet. Cloud cover outside thunderstorms was broken to overcast, and multilayered from 3,000 to 35,000 feet. Surface moisture helped produce low broken clouds west of the front in central Iraq: ceilings were 3,500 feet, with tops to 6,000feet. There were also broken middle clouds from 10,000 to 15,000 feet. Parts of south-central Iraq and north-central Saudi Arabia cleared as thunderstorms moved east.
Precipitation was moderate to heavy in thunderstorms, but light away from the strong cells.
Winds were east-southeasterly at 10-20 knots, becoming west-northeasterly at 10-25 knots as the storm moved through. Isolated thunderstorms were above 30 knots.
Visibilities were 9 km outside thunderstorms, but less than, 1,000 meters in heavy thundershowers. Blowing dust in areas along the front that had not received much rain lowered visibilities to 7 km. Evening fog formed along the Persian Gulf coast, lowering visibilities to 1,500 meters by 2300Z.
High temperatures ranged from 24 degrees Celsius in the southeast ahead of the cold front to as low as 15 degrees Celsius in the northwest behind it. Lows were 9 degrees Celsius in the north mid 14 degrees Celsius in the southeast.
21 February 1991
A low-pressure system moving south along the Persian Gulf neared Dhahran by 0300Z; by 1500Z, it was on the United Arab Emirates coast near 53 degrees East. Its cloudless cold front extended southwest across the Arabian Peninsula. By 0900Z, an area of high pressure had formed in northwestern Saudi Arabia near the Iraqi border
The low-pressure system spread a wide area of clouds. rain, and isolated thunderstorms over the Persian Gulf and along the coast as it passed. Ceilings were generally 10,000 feet in rainshowers, but ceilings in thunderstorms were reported at 3,000 feet. Inland, the front caused duststorms as it passed, reducing visibilities in some places to 800 meters. Fog blanketed northern Saudi Arabian the wake of the low-pressure system, but dissipated by 0800Z at most locations; visibilities were as low as 2,800 meters along the coast, but much lower in protected wadis. A long the eastern Saudi Arabian coast, visibilities were 4,800 meters in dense haze. Between 0500 and 1300Z, sporadic dust storms reduced visibilities to 6 kin in the Syrian Desert.
An overcast layer of low clouds resulted in 500-foot ceilings over Kuwait mid Iraq south of Baghdad. Cloud tops were about 1,200feet. The clouds lifted to 1,000-3,000 feet by 0500Z and dissipated by 0700Z. South of 29 degrees North, broken middle clouds with 10,000foot bases persisted until about 070OZ. Skies were clear after 0900Z.
Winds were northeasterly or northerly at 10 knots in the south, easterly at 10-15 knots in the north. Central Iraq's winds were light and variable. Highest speeds -- 20 knots along the northeastern Saudi Arabian border-- were reported at 150OZ.
Fog and visibilities of 500 meters were common. The fog dissipated in the northwest first, but lingered until 0800Z in Kuwait and Iraq south of 32 degrees North. Dense smoke reduced visibilities in southern Kuwait and northern Saudi Arabia. The afternoon high temperature was 15 degrees Celsius. Morning lows were 6-11 degrees Celsius, but by evening, temperatures in the north had fallen to about 3 degrees Celsius.
Visible Smoke PlumesDMSP visual imagery in Gulf War Weather shows smoke plumes in southern Kuwait extending southward into Saudi Arabia.
22 February 1991
High pressure was centered over east-central Saudi Arabia. A cold front extending from a low in the eastern Mediterranean spread scattered to broken high clouds across Syria and northwestern Iraq. The system had moved into eastern Syria by 1600Z. A low -pressure system near the Strait of Hormuz brought low cloudiness and rain to the southeastern Arabian Peninsula
A dense band of smoke aloft extended from the northern Persian Gulf along the Saudi Arabian coast into the Rub al Khali. Bases were about 10,000 feet, tops to 18,000 feet. Skies were clear to scattered, but scattered to broken middle and high clouds moved over the extreme northeastern by 1800Z. Ceilings, where present, were 10,000 feet with tops to 15,000 feet. The middle and high clouds were nearing Baghdad by 2300Z.
Visibilities were unrestricted except for areas affected by smoke, where they were generally about 6 km. Pilots reported smoke tops to about 15,000 feet and in flight visibilities as low as 1,000 feet. Dense smoke over and south of Kuwait
Winds were light and variable before 1500Z, becoming southeasterly to easterly at 5-10 knots to the east of the front after 150OZ. Elsewhere, winds remained light. After sunset, winds were newly calm. High temperatures were 13-18 degrees Celsius; lows, 1-8 degrees Celsius. The lowest temperatures were in the eastern Nafud Desert.
Visible Smoke Plumes
NOAA visual imagery in Gulf War Weather shows smoke plumes visible over Kuwait moving southward over coastal Saudi Arabia.
23 February 1991
High pressure centered over the eastern Arabian Peninsula moved southeastward into the Rub al Khali by 2000Z. Even though the frontal system dissipated as it moved across northwest Saudi Arabia, it still caused isolated light showers and duststorms. The subtropical jet stream brought middle and high clouds eastward over the area after 0900Z. Low pressure formed over the Red Sea
Fog reduced visibilities along the central Persian Gulf to about 1,000 meters between 0100 and 040OZ and reformed after 2000Z. Scattered to broken low and middle clouds with light isolated rainshowers reduced visibilities to 10 km along the weak low-pressure system in the west. Duststorms caused 4,000 meter visibilities in the Syrian and Nafud Deserts between 0900 and 1700Z. Middle and high clouds produced 10,000 foot ceilings over northwestern Saudi Arabia after 0900Z. Smoke from the Kuwaiti oilfields had reached Qatar, although concentrated at 10,000-12,000 feet, the smoke mixed with haze at lower levels to produce 6-km visibilities.
In the west, the low-pressure system caused scattered to broken clouds at 10,000 feet until about 060OZ, when they became scattered. By 120OZ, middle and high clouds began to move into the area south of 31 degrees north, causing broken to ceilings at 10,000 to 12,000feet. These clouds were east of 45 degrees East by 190OZ. Between 0400 and 160OZ, another band of middle and high clouds formed along the Iran-Iraq border north of 32 degrees North. Ceilings were about 8,000 feet, with tops to 32,000 feet. Isolated thunderstorms formed over Kuwait by 200OZ, with 2,500 foot bases and tops to 35,000 feet.
Winds were northerly to northwesterly at 10-15 knots East of 45 degrees east. Elsewhere, winds were easterly of 5-10 knots. Duststorms reduced visibilities to 8 km along the Iraq-Saudi Arabia border between 0800 and 150OZ. Dense smoke covered eastern Kuwait and reduced visibilities generally to less than 8 km, with isolated cases as low as 1,000 meters. High temperatures were 13-16 degrees Celsius, lows, 7-13 degrees Celsius.
24 February 1991
A low-pressure system moved slowly eastward along the Iraq-Saudi Arabia border. High pressure was still centered over the Southeastern Arabian Peninsula. The subtropical jet stream's middle and high clouds moved eastward over the Persian Gulf. They were out of the area by about 1900Z, but another upper-level disturbance brought more high and middle clouds eastward. At 1500Z, these clouds were in north-central Saudi Arabia.
Morning fog again blanketed the central Persian Gulf coast between Dhahran and the Strait of Hormuz. Visibility was poorest (2,000 meters) south of Qatar. Gust winds and blowing dust accompanied the low near the northern Saudi Arabian border where 15- to 20-knot winds raised dust that reduced visibilities to 6 km. Broken to overcast middle cloudy produced 8, 000 foot ceilings over the northern Persian Gulf but embedded low clouds resulted in isolated ceilings at 3,000 feet. Isolated rainshowers fell near the low, reducing visibilities to 8 km. Isolated thunderstorms, with bases at 2,500 feet and tops to 30,000feet, developed southwest of Riyadh between 1500 and 2200Z. Smoke reduced visibilities and obscured skies along the Persian Gulf as far south as 23 degrees North.
In Kuwait and southern Iraq, skies were broken overcast with 8,000 foot ceilings until about 0500Z. Tops of these multilayered clouds reached 35,000 feet. There were isolated 2,500-foot ceilings. By 0500Z, the higher clouds had moved east, leaving scattered to broken low clouds over Kuwait. In the evening, more middle and high clouds began to move into the southern half from the west. They reached western Kuwait by 2000Z, bringing 9,000-foot ceilings and tops to 30,000 feet.
Isolated Rainshowers and thunderstorms affected Kuwait and southeastern Iraq until 060OZ. Rain, heavy at times, reduced visibility to 5 km. Winds in Saudi Arabia end western Iraq were southwesterly to westerly at 10-15 knots, increasing to 15-25 knots by 0900Z south of 32 degrees North, with gusts to 30 knots. By 2100Z, speeds had diminished to 10-15 knots. Winds in the Tigris-Euphrates river valley were southeasterly at 10-20 knots, but dropped to 3-5 knots after sunset.
Dust storms reduced visibilities to as low as 1,000 meters in Kuwait and southern Iraq between 0900 and 2100Z. Dense smoke from the Kuwaiti oil fires moved northwestward. Visibilities just south of Baghdad were less than 3,000 meters. Fog formed after 2100Z in Kuwait and southern Iraq, reducing visibilities to less than 4,000 meters. Afternoon high temperatures were 10-21 degrees Celsius; morning lows ranged from 1 degree Celsius in the northeast to 15 degrees Celsius in the southeast.
Visible Smoke Plumes
DMSP visual imagery in Gulf War Weather shows smoke plumes from Kuwait moving westward into Iraq.
(As the ground war began, Iraqi forces set fire to Kuwaiti oil wells, resulting in extremely heavy smoke concentrations over the entire region.)
25 February 1991
An upper-air disturbance moving northeastward spread stormy weather over the northern Arabian Peninsula; by 0900Z, most of the region was covered with clouds. A low-pressure system lingered over northwestern Saudi Arabia as the high-pressure cell in the southeast moved eastward. Low pressure moving east from the northeastern Mediterranean spread clouds southeastward over northern Iraq.
Fog reduced visibilities to as low as 1,500 meters from northeastern Saudi Arabia to the United Arab Emirates coast (and to as low as 500 meters in the Tigris-Euphrates river valley) before 0400Z and again after 2000Z. Broken middle and high multilayered clouds with tops to 30, 000 feet spread 9, 000-foot ceilings from the northern Red Sea to the northern Persian Gulf and along the Iran-Iraq border. Isolated thunderstorm s and rainshowers formed over northwestern Saudi Arabia throughout the day. They were most intense and widespread at about 1600Z northwest of Riyadh, along the southern Iraq-Iran border, and in extreme western Iraq near the Jordan border. Some of these storms were dry, creating intense, localized duststorms that reduced visibilities to well below 1,000 meters. Widespread duststorms were reported in the northern Arabian Peninsula and the Syrian Desert between 0900 and 2000Z with visibilities as low as 4,000 meters. Prevailing winds were as high as 30 knots in northeastern Saudi Arabia
At 0300Z, broken high clouds with 24, 000-foot ceilings prevailed over Iraq and Kuwait; but as denser clouds continued to move in, a solid overcast from 7,000 to 33,000 feet formed throughout southern Iraq and Kuwait. After 1300Z, isolated thunderstorms with tops to 35,000 feet developed in the area's southern half; skies in the heaviest storms were obscured. Conditions over southern Iraq and Kuwait improved after 1800Z. In southwestern Iraq between the Tigris River and the Iranian border, skies were scattered with isolated low clouds from 2,000 to 20,000 feet. South of 30 degrees North, skies were broken to overcast with 20,000-foot ceilings; there were also isolated low clouds from 10,000 to 35,000 feet. Elsewhere, skies remained overcast between 8,000 and 35,000 feet.
At 0500Z, a line of rainshowers spread from west-central Saudi Arabia northeastward to the Saudi Arabia-Iraq border and eastward into southern Kuwait. The line expanded and intensified to cover most of Kuwait, southern Iraq, and north central Saudi Arabia by 1600Z. Intermittent precipitation fell the test of the .
Winds were southeasterly at 5-10 knots until 0900Z. Afternoon winds were stronger at 15-20 knots, with gusts to 40. Fog and smoke reduced visibilities to below 2,000 meters in southern Iraq and Kuwait. Visibilities improved to 8 km by 0600Z, but sporadic dust storms in the afternoon reduced them to 4,000 meters. High temperatures were 14-21 degrees Celsius; lows, 3-16 degrees Celsius.
26 February 1991
As the upper-air disturbance moved northeast, it continued to produce heavy rainshowers and dust storms over the area. A surface trough formed between the low pressure area in central Saudi Arabia and another moving through southern Turkey. By 2100Z, the trough stretched through Iraq along 43 degrees east. An area of high pressure was located in central Iran and the extreme southeastern Arabian Peninsula
Several lines of rainshowers and thunderstorms moved through the northern Arabian Peninsula throughout the day. Between 0000 and 0300Z, an area of thunderstorms spread from the Red Sea near 25 degrees North to the lraq-Saudi Arabia border near 45 degrees East. Another formed in northeastern Iraq near the Iranian border. By 0900Z, a third area had formed over northeastern Saudi Arabia at 28 degrees North, 47 degrees East. Bases were at 2,500 feet and tops reached 35, 000 feet. Thunderstorms were embedded in scattered to broken middle clouds west of 45 degrees East. Multilayered clouds were broken to overcast from 8. 000 to 33, 000 feet north of 25 degrees North. By 1100Z, the northern area had spread southwestward and the southern areas had moved southeastward. Storm intensity and coverage increased throughout the day until 1600Z, when a line of isolated thunderstorms extended from the northern Persian Gulf to southwest of Riyadh. Areas west of 43 degrees East had cleared. Clouds, rainshowers, and thunderstorms spread southeastward again in the evening, reaching as far southwest as 20 degrees North, 44 degrees East, by 190OZ.
Broken to overcast clouds between 8,000 and 20,000 feet covered the entire area before 0300Z. The lower cloud deck gradually dissipated in the northwest, leaving scattered skies over most of Iraq, and high clouds with tops to 32,000 feet over southern Iraq and Kuwait. Scattered to broken clouds between 4,000 and 6,000 feet formed over central Iraq between 0500 and 1600Z. At 1100Z, there were isolated thunderstorms or rainshowers embedded in these clouds in a line from 35 degrees
North, 45 minutes East, to 31 degrees North, 41 minutes East. Thunderstorms also formed over eastern Kuwait and extreme southwestern Iraq after 1500Z. Cloud bases were 3,000 feet and tops reach 35,000 feet.
Intermittent rainshowers and thunderstorms fell southeast of a line extending from 34 degrees North, 46 minutes East, to 31 degrees North, 42 minutes East, throughout the day.
Winds were southeasterly at 10-15 knots, but by 1200Z, speeds in the east reached 20-30 knots. Winds in the west shifted to northwesterly at 10-15 knots as the trough moved eastward. Fog and smoke reduced visibilities to below 2,000 meters from the central Tigris-Euphrates river valley to Kuwait. Visibilities improved to 8 km by 060OZ, but sporadic dust storms in the afternoon reduced visibilities to 4,000 meters. Visibilities in heavy rainshowers may have dropped to as low as 1,000 meters. High temperatures were 17-21 degrees Celsius; lows, 7-16 degrees Celsius.
27 February 1991
A low-pressure cell that had been centered in southeastern Iraq at 1000Z slid southeastward into the Persian Gulf throughout the day. A weak frontal system in the eastern Mediterranean Sea moved onshore and was in central Iraq by the end of the day.
In western Iraq and northwestern Saudi Arabia, skies were scattered with bases at 10,000 feet throughout the morning. Clouds from the front approaching from the Mediterranean began moving in by 1100Z, forming ceilings rapidly. Rain began lowering visibilities to 5 km by 130OZ. Thunderstorms developed in the afternoon as the clouds moved eastward. By the end of the day, clouds and rain were confined to the western Saudi Arabia-Iraq border. In north-central and northeastern Saudi Arabia broken clouds, multilayered from 3,000 to 25,000 feet with rainshowers and thunderstorms, prevailed. Visibilities were 4,800 meters in ground fog, rain and haze, but near zero in blowing dust from thunderstorms. Clouds moved slowly southeast to east central Saudi Arabia by day 's end.
Broken multilayered clouds from 3,000 to 25,000 feet covered the southern half of the area, but cleared from the northwest by noon, leaving scattered clouds at 3,000 feet and broken clouds at 6,000-8,000 feet over southeast Iraq and Kuwait. These also cleared by 1900Z. A smoke layer at 2,500 feet covered most of central and southern Kuwait throughout the day. A line of broken 4,000-foot clouds associated with the from the Mediterranean invaded the western part of the area by noon. The line was past Baghdad and into north central Saudi Arabia by the end of the day. Rainshowers and thunderstorms were widespread in the southern half of the area through the morning. Light rain fell in the western half as the front passed.
Winds were northwesterly to northeasterly at 5-15 knots (but up to 25 knots in thunderstorms) in the southern half of the area. Winds became southwesterly at 5-15 knots as the front approached, and northwesterly at 8-20 knots behind it. Visibilities were near zero in dense fog along the Tigris-Euphrates river basin. There were also near zero in the southern half of the area where thunderstorms produced blowing dust. Elsewhere, morning visibilities were 5 km in ground fog, rain, and haze. Rain lowered visibilities to 4,800 meters in the western half of the area as the front passed. Smoke limited visibility aloft to 1,600 meters over Kuwait. High temperatures were 13-20 degrees Celsius; lows, 7-16 degrees Celsius.
28 February1991
Low pressure was centered over the southeastern part of the Saudi Arabian Peninsula while high pressure intensified in the rest of the region. Remnants of a weak frontal system remained in northern' Saudi Arabia and southern Iraq.
Skies were broken to overcast over north central northeastern, east, and east central Saudi Arabia. Ceiling heights were 3,000-4, 000 feet. By evening. skies were mostly clear to scattered. Light rain and drizzle fell over north-central and eastern Saudi Arabia. Thunderstorms with tops to 35,000 feet were observed over east-central Saudi Arabia and the northern part of the Persian Gulf during early morning. Winds were northwesterly at 10-20 knots with gusts to 25 knots. Fog lowered morning visibilities to 4,800 meters in east central Saudi Arabia. Fog reduced early afternoon visibilities to 3,200 meters in northeastern Saudi Arabia, which improved to 6-8 km in smoke and haze by late afternoon. A sandstorm in east central Saudi Arabia, with wind speeds of 30-40 knots, reduced late afternoon and many evening visibilities to 1,600-4,000 meters, with isolated reports of 100 meters.
Skies were broken to overcast over southern and southeastern Iraq and Kuwait -- ceilings were 3,000 to 4,000 feet, but 800 feet in showers. By early evening, skies were clear to scattered. Isolated afternoon thunderstorms (tops to 35,000 feet) and rainshowers were present over southeastern Iraq and Kuwait.
Winds were northwesterly to northerly 41 10-20 knots, with gusts to 35 knots near thunderstorms. In Kuwait, visibilities were less than 3,200 meters in smoke and 2,000 meters in thunderstorms. High temperatures were 13-18 degrees Celsius, lows, 5-10 degrees Celsius.
1 March 1991
High Pressure dominated, but a low-pressure system developed over the eastern Mediterranean by the end of the day. sending moisture into western areas. Skies were clear to scattered over in most of the area but scattered to broken at 1,000-2,000 feet over northeastern and eastern Saudi Arabia due to smoke. Scattered to broken low clouds at 3,000 feet, with occasionally broken middle and high ceilings, moved into western Iraq and northwestern Saudi Arabia by mid-afternoon. Winds were northwesterly to northerly at 10-15 knots. Visibilities in northeastern Saudi Arabia were 6-8 km in smoke and haze. Blowing sand and dust reduced early morning visibilities to 3,200 meters in east-central and eastern Saudi Arabia. Scattered, occasionally broken, middle clouds at 8,000- 10,000 feet moved into central Iraq by mid-afternoon.
Winds were northwesterly at 10-15 knots. Smoke and haze reduced visibilities in Kuwait to 5-7 km, occasionally to 3,200 meters. High temperatures were 15-20 degrees Celsius; lows, 5-10 degrees Celsius.
2 March 1991
High pressure dominated as a low-pressure system moved northeast and brought moisture across Iraq and northern Saudi Arabia. Skies were broken to overcast at 8,000-10,000 feet, but early morning ceilings were 3,000-5,000 feet in showers over western and northern Iraq. Smoke formed a broken layer at 2,000-3, 000 feet over northeast and east central Saudi Arabia during the morning. Skies over the rest of the area were clear to scattered. Isolated rainshowers and thunderstorms with tops to 35, 000 feet developed during early morning in northern Iraq. Visibilities were 6-8 km in precipitation. Haze reduced morning visibilities to 4,800 meters in east-central Saudi Arabia. Smoke reduced morning visibilities in eastern Saudi Arabia to 4,800 meters; in the afternoon and evening, to 4,000 meters.
Over central Iraq, skies were broken with middle clouds at 8, 000-10,000 feet in the early morning, becoming scattered in early afternoon. Winds were northwesterly at 10-15 knots. Smoke reduced visibilities in Kuwait to 5-7 km, with isolated areas of less than 1,600 meters. High temperatures were 15-20 degrees Celsius; lows, 5-10 degrees Celsius.
Conclusions
The following facts provide significant evidence that coalition forces were exposed to mixed chemical agents as a result of coalition bombings of Iraqi nuclear, chemical, and biological facilities and that the fallout from these bombings may be contributing to the health problems currently being suffered by Gulf War veterans.
Iraqi nuclear, chemical, and biological weapons plants and storage sites were priority targets for U.S. and Coalition forces and were repeatedly bombed.
Chemical alarms began sounding and the servicemen were put on chemical alert simultaneous with the beginning of the air war.
The nature of diesel, oil, etc., did not alter during the air war, suddenly causing the alarms to sound. These substances were present before the initiation of the air war, and did not set off the chemical alarms. (The automatic alarms have no sensitivity control.)
These chemical alarms are battlefield instruments. Battlefields are full of fumes, propellant , explosives, and so forth. It is difficult to believe that they would have been procured if they were ineffective in this environment.
U.S. Military personnel, and the Czech and French governments have confirmed that the chemical alarms were sounding as the result of nerve agent detection.
The combination of prevailing wind directions, the open terrain, the lack of structural impediments, and other factors listed above, indicate that chemical and possibly nuclear and biological agents from allied bombings became airborne and were being blown and carried across coalition forces emplacements along the Saudi-Iraqi and Saudi-Kuwaiti border.
Chemical nerve agents, such as Sarin and others, are known to have a cumulative effect, i.e., they have a slow rate of detoxification. Little is known about the long-term effects of continuous low levels of exposure. Many of the veterans claiming to be suffering from Gulf War Syndrome are exhibiting symptoms of neurophysical disorders.
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