Mountains receive more rainfall than low lying areas because as air is forced over the higher ground it cools, causing moist air to condense and fall out as rainfall. The higher the place is above sea level the colder it will be.
How does Relief Act as a climate control?
Relief : It plays a major role in determining the climate of a place. High mountains act as barriers for cold or hot winds. They may also cause precipitation.
How does relief features affect climate?
Relief plays a major role in determining the climate of a place. High mountains act as a barriers for cold or hot winds; they may also cause precipitation if they are high enough and lie in the path of rain-bearing winds. The leeward side of mountains remains relatively dry.
How does relief mountains affect climate?
The relief of mountains affects climate because they stand in the path of wind systems and force air to rise over them. As the air rises it cools, leading to higher precipitation on windward mountain slopes (orographic precipitation); as it descends leeward slopes it becomes warmer…
How does relief play a major role in determining the climate of a place?
Relief has a great bearing on the climate of a place . The higher the place,the cooler it is and lower the place,the hotter it is because the temperature decreased at the rate of 1 degree celcius for every 165 metres. That is how relief play a major role in determining the climate of a place.
How does relief act as a climatic control class 9?
As the distance from the sea increases the weather conditions become extreme. Places away from the sea have very hot summers and very cold winters. … Another major control of climate is the relief of a place. Mountains often act as natural barriers for wind and moisture, affecting the climate of the areas around it.
How does the relief of an area affect the climate of a place Class 9?
Answer: The relief of a place affects the climate of a place when the high mountains act as barriers for cold and hot winds, e.g. the Himalayas. They also affect the amount of rainfall if they are very high. They force the wind to give heavy rain on the windward side and less rain on the leeward side.
How does relief features affect climate of Asia?
Mountain Ranges: The mountain ranges of Asia running in the east west direction obstruct the path of rain bearing winds coming from the south and bring rain to the areas which lie on the windward side of the mountains. Further, the Himalayas act as a barrier to the cold winds rising from Central Asia.
How does the relief affect the climate of India western Rajasthan receives very little rainfall?
Answer: Rajasthan gets scanty rainfall because the state lies in the rain shadow region of the Aravali Range. The Aravali Range lie parallel to the Arabian Sea branch of South West Monsoon and do not offer any obstruction to the rain bearing winds. … Only north Gujarat receive scanty rainfall).
What are relief features?
relief features are those features which are related to landscape of those areas, eg. mountains, altitude, valleys, types of land and heights of mountains.
How does topographic relief influence the weather?
Land: Climate and Temperature. The topography of an area also helps determine the climate. This is because of ocean currents that carry masses of warm or cool air to coastal locations. … Areas near oceans and large lakes have smaller temperature ranges than landlocked, or continental, areas.
How do mountains affect climate and weather?
Mountains can have a significant effect on rainfall. When air reaches the mountains, it is forced to rise over this barrier. As the air moves up the windward side of a mountain, it cools, and the volume decreases. As a result, humidity increases and orographic clouds and precipitation can develop.
What is relief land features?
India has land under a variety of relief features, namely; mountains, plateaus, plains and islands. About 43 per cent of the land area is plain, which provides facilities for agriculture and industry. … About 27 per cent of the area of the country is the plateau region.