Server processing time: The last factor in the response time formula is the processing time required by the server and the client to put together [i.e. generate and render] the required page so it can be viewed by the requester. This can vary dramatically for different types of Web pages.
1 The climate in South-East Asia, India and across the Indian Ocean is dominated by torrential monsoon rains. 2  Monsoons also affect parts of Africa and South America.3  The savannas regions of the world, the most extensive of which are in Africa, also have very pronounced wet and dry seasons. The climate in South-East Asia, India and across the Indian Ocean is dominated by torrential monsoon rains. 2  Monsoons also affect parts of Africa and South America.
All of these prevailing winds help generate the rain shadow effect that is commonly found around the world. Examples of Rain Shadow Areas. In Asia, the Himalaya mountain range acts as the catalyst for the rain shadow effect over the Tibetan Plateau, Central Asia, and the Gobi Desert. The Japanese Alps create that same phenomenon over the Kanto Plain in the Tokyo region. The Arakan Mountains also have that effect over the central regions of Myanmar.