Temperature and precipitation vary from place to place and season to season. Explain by giving examples.
Answers
Answer:
yes it is true....
Explanation:
1 In summer the Mercury occasionally touches 50 degree Celsius in some parts of Rajasthan desert where is it maybe celsius in pahalgam in Jammu and Kashmir.
2. On a winter night temperature address in Jammu and Kashmir may be as low as minus 45 degree Celsius. Thiruvananthapuram on the other hand may have temperature of 22 degree Celsius.
3. The annual precipitation varies from over 400 centimetre in meghalaya to less than 10 centimetre in ladakh and western Rajasthan.
4. Most parts of the country receive rainfall from June to September but some parts, like tamilnadu coast gets a large portion of rainfall during October and November.
5. While precipitation is mostly in the form of snowfall in a part of Himalayas, it rains over the rest of the country.
6. Coastal areas experience less contrast in the temperate condition . Seasonal contrast are more in the interior of the country. there is a decrease in rainfall generally from east to west in the northern plains.
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Answer:
The temperature and precipitation varies from one place to another because of their different location on map/globe.
Explanation:
Temperature and precipitation vary from place to place and from season to season. In the regions where the sky is covered with cloud or where the rains are falling or the summer temperature is relatively lower.
But during the winter, by terrestrial radiation. the clouds check the loss of heat.
Temperature vary from place to place
The temperature varies from one place to another because of their different location on map/globe. If they location are near equator they may have humid and hot type of climate and if the place is more towards poles the place is not as hot as compared to the equator one.
Precipitation vary from place to place
High rainfall amounts is recieved by the areas near the equator receive because constant solar heating produces large-scale evaporation, intense heating, moist rising air that forms convectional rainfall and cools with altitude .Also, air masses converging takes place which results in heavy rainfall.
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