In the area of the tropical daytime climates of Southeast Asia, however, the temperatures are hardly subject to seasonal fluctuations. The altitude dependence of the temperature becomes clear in the area of the Himalayas; the high mountain region emerges as a cold island in the map both in summer and in winter.
Asia – annual rainfall
The distribution of precipitation over Asia shows a trend from the constantly humid tropics to the interior of the continent. In large parts of Southeast Asia and India, the highest values in Asia are reached with annual precipitation of 1,000 to 3,000 millimeters. In Central Asia, the increasing hygric continentality and the leeward location to the Himalayas mean that precipitation is falling to less than 100 millimeters in some cases (Gobi Desert). In the Arab region, the influence of the descending air masses of the subtropical high pressure belt is very noticeable and there, too, leads to annual rainfall of 100 millimeters and below. For more information about the continent of Asia, please check ezinereligion.com.