Roughly 90 percent of the annual rainfall occurs between November and April, most of it in the winter months from December through March. The remaining six months, particularly the hottest ones of June, July, and August, are dry.

Except in the north and northeast, mean annual rainfall ranges between ten and seventeen centimeters. Data available from stations in the foothills and steppes south and southwest of the mountains suggest mean annual rainfall between thirty-two and fifty-seven centimeters for that area. Rainfall in the mountains is more abundant and may reach 100 centimeters a year in some places, but the terrain precludes extensive cultivation. Cultivation on nonirrigated land is limited essentially to the mountain valleys, foothills, and steppes, which have thirty or more centimeters of rainfall annually. Even in this zone, however, only one crop a year can be grown, and shortages of rain have often led to crop failures.

Mean minimum temperatures in the winter range from near freezing (just before dawn) in the northern and northeastern foothills and the western desert to 2o-3° C and 4o-5° C in the alluvial plains of southern Iraq. They rise to a mean maximum of about 15.5° C in the western desert and the northeast, and 16.6° C in the south. In the summer mean minimum temperatures range from about 22.2° C to about 29° C and rise to maximums between roughly 37.7o and 43.3° C. Temperatures sometimes fall below freezing and have fallen as low as -14.4° C at Ar Rutbah in the western desert. They are more likely, however, to go over 46° C in the summer months, and several stations have records of over 48° C.

The summer months are marked by two kinds of wind phenomena. The southern and southeasterly sharqi, a dry, dusty wind with occasional gusts of eighty kilometers an hour, occurs from April to early June and again from late September through November. It may last for a day at the beginning and end of the season but for several days at other times. This wind is often accompanied by violent duststorms that may rise to heights of several thousand meters and close airports for brief periods. From mid-June to mid-September the prevailing wind, called the shamal, is from the north and northwest. It is a steady wind, absent only occasionally during this period. The very dry air brought by this shamal permits intensive sun heating of the land surface, but the breeze has some cooling effect.

The combination of rain shortage and extreme heat makes much of Iraq a desert. Because of very high rates of evaporation, soil and plants rapidly lose the little moisture obtained from the rain, and vegetation could not survive without extensive irrigation. Some areas, however, although arid do have natural vegetation in contrast to the desert. For example, in the Zagros Mountains in northeastern Iraq there is permanent vegetation, such as oak trees, and date palms are found in the south.

Data as of May 1988

NOTE: The information regarding Iraq on this page is re-published from The Library of Congress Country Studies and the CIA World Factbook. No claims are made regarding the accuracy of Iraq Climate information contained here. All suggestions for corrections of any errors about Iraq Climate should be addressed to the Library of Congress and the CIA.