With the exception of the desert region in western India, the seasonal monsoon patterns heavily influence rainfall, and when that rainfall occurs. Most of India experiences high rainfall, particularly in the summer months. The height of the Himalayan Mountains concentrates most of the monsoonal rainfall on the Indian Subcontinent. This same mountain range blocks cold winds from Siberia from penetrating the region.
This is why most of India has a warm, tropical climate with high precipitation. Conversely, the regions north of the Himalayas are much colder and drier. Western China and Mongolia are examples of a cold desert climate. These are regions of very little rainfall and bitterly cold winters. The high latitude and elevation of Mongolia and western China are responsible for the cold winters in these areas. China's Taklamakan Desert is much hotter during the summer as elevations are lower than found in Mongolia.
Being north of the mountain range and north of the Tibetan Plateau , bitterly cold winter winds influenced by the Siberian High Pressure system can blow through the region unmitigated. The Himalayas also create a rain shadow. Rain from the summer monsoons cannot easily penetrate the mountains.
The monsoon winds from South Asia cannot easily reach regions north of the Himalayas. Thus, the reason why the Taklamakan and Gobi deserts exist.
Seasonal monsoons, latitude, and elevation play major roles in shaping the climate in Asia. The Himalayas have a profound effect on the climate of the Indian subcontinent and the Tibetan Plateau. They prevent frigid, dry winds from blowing south into the subcontinent, which keeps South Asia much warmer than corresponding temperate regions in the other continents.
The Himalayas play a very important role in influencing the climate of India. India is a monsoon land only because of the presence of Himalayas. It traps the monsoon winds from Arabian sea and Bay of Bengal and forces them to shed their moisture content within the Indian sub-continent in the form of snow and rain. Since the weather conditions are very different depending on where the Himalayas are in relation to where you want to live, this would probably be the most important feature to consider.
Its indigenous cultures pioneered many practices that have been integral to societies for centuries, such as agriculture, city planning, and religion.
The social and political geography of the continent continues to inform and influence the rest of the world. Asia is the most important region of our world for achieving global well-being. One reason is simply the region we call Asia is where most of us live. In being so populous, Asia is also home to diverse societies, each with their own creativity and technological prowess.
Studying the culturally and historically diverse areas of Asia provides opportunities for students to discover new global perspectives. Economic transformations in Asia have reshaped our global economic and political environment. The Sumerian civilization is the oldest civilization known to mankind. The term Sumer is today used to designate southern Mesopotamia. In BC, a flourishing urban civilization existed. The Sumerian civilization was predominantly agricultural and had community life.
Only four ancient civilizations—Mesopotamia, Egypt, the Indus valley, and China—provided the basis for continuous cultural developments in the same location. A civilization is often defined as a complex culture with five characteristics: 1 advanced cities, 2 specialized workers, 3 complex institutions, 4 record keeping, and 5 advanced technology.
These include: 1 large population centers; 2 monumental architecture and unique art styles; 3 shared communication strategies; 4 systems for administering territories; 5 a complex division of labor; and 6 the division of people into social and economic classes.
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