Most of Asia is in the Northern Hemisphere. However there are some small islands that are part of Asia, however lie south of the equator. So they are in the Southern Hemisphere. There are also parts of Asia that lie in the Eastern Hemisphere. However, the majority of the continent lies in the Northern Hemisphere.
Answer:
Trade wind blows from the east to the west direction
Explanation:
The trade winds are usually defined as those wind that blows from the tropics of both the hemisphere and moves towards the equator. They originate from the northeastern and southeastern direction in the northern and southern hemisphere respectively.
This wind blows from the east to the west, and as it blows it carries the hurricanes and other types of cyclones. It helps in increasing the growth and strength of hurricanes. The intensity of the trade wind decreases as the hurricane moves over the vast oceans and reaches the land areas or the continent.
Answer:
Leeward
Explanation:
Mountains can act as a climatic barrier by blocking prevailing winds and trade winds from getting to the other side of the mountain.
The area that faces the winds is called the windward side. This side receives most of the moisture picked up by the winds from the oceans. This is why it is wetter on this side.
The LEEWARD side is a lot drier because the mountain blocks most of it and as the winds climb up the mountain, most of the moisture is well spent and fall on the windward side. By the time the wind gets to the other side of the mountain, they are dried up already. The <u>leeward</u> side is the area that faces away from the wind.
Answer:
The Milankovitch cycles in association with other natural factors explain how glaciers may advance and retreat over periods of d. ten thousand to one hundred thousand years.
Explanation:
The Milankovitch cycles -
This is the movement related to Earth's orbit around the Sun .
There are three cycles , Axial tilt , Eccentricity and precession .
According to this theory , these cycles together affect the amount of the solar heat that is incident towards the Earth's surface and the climatic pattern .
The Milankovitch cycle helps the advance and retreat of ice over the periods of 10,000 to 1000,000 years , but it does not explain the cause of Ice Age.
