Iraq has many different climates, but is dominated by BWh.
The mountains in the northeast are an extension of the alpine system that runs eastward from the Most geographers, including those of the Iraqi government, discuss the country's geography in terms of four main zones or regions: the Because the waters of the Tigris and Euphrates above their confluence are heavily The Tigris and Euphrates also carry large quantities of Between Upper and Lower Mesopotamia is the urban area surrounding The northeastern highlands begin just south of a line drawn from The desert zone, an area lying west and southwest of the Euphrates River, is a part of the Western and southern Iraq is a vast desert region covering some 64,900 square miles (168,000 square km), almost two-fifths of the country. Al-Dibdibah is a more sandy region with a covering of scrub vegetation. Precipitation may exceed 40 inches (1,000 mm) in the mountains, much of which falls as snow. It’s punishingly hot. A such summer heat, even in a hot desert, is high and this can be easily explained by the very low elevations of deserts regions which experience these exceptionally searing high temperatures. The pattern holds for farming communities in the Fragmentary information suggests that most farmers in the alluvial plain tend to live in villages of over 100 persons. Winters can be cold because of the region’s high relief and the influence of northeasterly winds that bring continental air from In the foothills of the northeast, annual precipitation of 12 to 22 inches (300 to 560 mm), enough to sustain good seasonal pasture, is typical. The rivers are at their lowest level in September and October and at flood in March, April, and May when they may carry forty times as much water as at low mark. The climate is influenced by Iraq's location between the subtropical aridity of the Arabian desert areas and the subtropical humidity of the Persian Gulf.
Some areas, however, although arid, do have natural vegetation in contrast to the desert.
Both deserts are part of the Arabian Desert.
Elevation in the southern desert averages between 1,000 and 2,700 feet (300 to 800 metres). Except in the north and northeast, mean annual rainfall ranges between 100 and 190 millimeters (3.9 and 7.5 in). the swamps act as silt traps, and the Shatt al Arab is relatively silt free as it flows south. Iraq Climate . Temperatures sometimes fall below freezing and have fallen as low as −14 °C (6.8 °F) at Ar Rutbah in the western desert. Close to the coast and along the Shatt al-Arab (known as arvandrūd: اروندرود among Iranians) there used to be marshlands, but many were drained in the 1990s. Moreover, one season's flood may be ten or more times as great as that in another year. The average temperatures in Iraq range from higher than 48 degree C (120 Fahrenheit) in July and August to below freezing in January. Articles from Britannica Encyclopedias for elementary and high school students.
Al Hajarah has a complex topography of rocky desert, wadis, ridges, and depressions. Data available from stations in the foothills and steppes south and southwest of the mountains suggest mean annual rainfall between 320 and 570 millimeters (12.6 and 22.4 in) for that area. Classifications. With much of the fighting concentrated in their areas, they have either migrated to settled communities away from the marshes or have been forced by government decree to relocate within the marshes. In the summer mean minimum temperatures range from about 27 to 31 °C (80.6 to 87.8 °F) and rise to maxima between roughly 41 and 45 °C (105.8 and 113.0 °F). The summer is generally dry and hot, but average temperatures are some 5–10 °F (3–6 °C) cooler than those of lowland Iraq. Our editors will review what you’ve submitted and determine whether to revise the article.Iraq has two climatic provinces: the hot, arid lowlands, including the alluvial plains and the deserts; and the damper northeast, where the higher elevation produces cooler temperatures. In the rural areas of the alluvial plain and in the lower Diyala region, settlement almost invariably clusters near the rivers, streams, and irrigation canals. Summer, which lasts from In winter the paths of westerly atmospheric depressions crossing the In the northeast the summer is shorter than in the lowlands, lasting from June to September, and the winter considerably longer. Averages high temperatures are generally above 40 °C (104 °F) at low elevations during summer months (June, July and August) while averages low temperatures can drop to below 0 °C (32 °F) during the coldest month of the year during winter The all-time record high temperature in Iraq of 52 °C (126 °F) was recorded near An Nasiriyahon 2 August 2011.
The southern and southeasterly The combination of rain shortage and extreme heat makes much of Iraq a desert. For example, in the mid-1970s a substantial number of the residents of The Marsh Arabs of the south usually live in small clusters of two or three houses kept above water by The war has had its effect on the lives of these denizens of the marshes. It has been recognized since 1913 as the boundary between western The Euphrates originates in Turkey, is augmented by the Both the Tigris and the Euphrates break into a number of channels in the marshland area, and the flow of the rivers is substantially reduced by the time they come together at Al Qurnah. In 1954, for example, Baghdad was seriously threatened, and Until the mid-twentieth century, most efforts to control the waters were primarily concerned with irrigation.
A majority of … Classification …
Annual Weather Averages Near Baghdad. The war has also affected settlement patterns in the northern In the arid areas of Iraq to the west and south, cities and large towns are almost invariably situated on watercourses, usually on the major rivers or their larger tributaries. For example, in the In 1922 British officials concluded the Treaty of Mohammara with Abd al Aziz ibn Abd ar Rahman Moreover. Also, in early 1988, the marshes had become the refuge of deserters from the Iraqi army who attempted to maintain life in the fastness of the overgrown, desolate areas while hiding out from the authorities. Rainfall in the mountains is more abundant and may reach 1,000 millimeters (39.4 in) a year in some places, but the terrain precludes extensive cultivation.