The seasonal reversal of wind direction associated with large continents is called a monsoon. This phenomenon is characterized by the shift in prevailing wind patterns, bringing heavy rainfall during specific times of the year.
It is called a "monsoon." Monsoons are characterized by a seasonal reversal of wind direction that brings large amounts of rainfall to certain regions.
The temperate zone includes North America, Europe, Asia (parts of Russia), South America, Australia, and Africa (parts of South Africa, southern parts). These continents experience moderate temperatures and distinct seasonal changes.
The type of climate found in the interior of the major continents in the middle, or temperate, latitudes. The climate is characterized by a great seasonal variation in temperatures, four distinct seasons, and a relatively small annual precipitation.
Seasonal winds are prevailing wind patterns that change direction in a predictable manner depending on the time of year. They are caused by temperature differences between land and sea, leading to the movement of air masses. Examples include the monsoon winds in South Asia and the trade winds in tropical regions.
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Seasonal wind direction http://answers.yahoo.com/question/index;_ylt=ArE8pJxS106Jhh7ccnTOEUYjzKIX;_ylv=3?qid=20080804201130AAES2mR
seasonal reversal of winds
A monsoon is a strong wind that blows from one direction in winter and the opposite direction in summer. This seasonal change in wind direction is due to the difference in temperature between the land and sea, causing a reversal in the wind pattern.
The monsoon wind is a seasonal wind pattern that brings heavy rainfall to certain regions. It occurs primarily in South and Southeast Asia, where the wind direction changes with the shift in pressure systems, leading to wet summers and dry winters.
It is called a "monsoon." Monsoons are characterized by a seasonal reversal of wind direction that brings large amounts of rainfall to certain regions.
India
milipary
A wind that changes direction with the seasons is known as a seasonal wind or monsoon. Monsoons are characterized by a reversal in wind direction due to differential heating and cooling of land and sea surfaces. They typically bring heavy rainfall during one season and dry conditions during another, impacting various regions around the world, such as South Asia and parts of Africa.
The wind system that reverses its direction seasonally is the monsoon. In regions affected by monsoons, such as South Asia, the winds blow from the sea to the land during the summer, bringing heavy rains, and shift to blowing from the land to the sea during the winter, resulting in dry conditions. This seasonal reversal is primarily driven by temperature differences between land and ocean.
During the winter Asia becomes cold creating high pressure which directs surface flow off the land. The opposite occurs in the summer where a low settles over the land bringing air from the ocean to flow over land. The wind reversal is known as a monsoon.
Monsoons are caused by the seasonal reversal of wind patterns, which brings heavy rainfall to certain regions. In the case of the Indian subcontinent, for example, monsoons occur when warm, moist air from the Indian Ocean moves inland due to a shift in wind direction. This phenomenon leads to a wet summer season in the region.
Yes, the seasonal shift of isotherms is greater over continents than over oceans. This is because land heats up and cools down faster than water due to differences in heat capacity. As a result, the temperature difference between summer and winter is more pronounced over continents, leading to larger shifts in isotherms.