♦ Why does the Alaskan coast remain ice-free in winter ?
♦ Why are slanting rays less effective in heating the atmosphere than vertical rays?
♦ Differentiate between Cyclonic rainfall and Convectional rainfall
Answers
Answer:
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Explanation:
1.In this way,warm currents along the coast make the coastal areas warmer and cold currents make them cooler than usual. ... The parts of western Europe remains ice free during winter.
2.Vertical rays heat up a smaller surface. ... Vertical rays travel through a shorter distance in the atmosphere and the loss of heat is less. Slanting rays travel a longer distance through the atmosphere where much of its heat is absorbed by clouds, water vapour and dust particles.
3.Convectional rainfall: When the temperatures are high, the air gets heated. Warm air rises higher into the atmosphere; it then expands and spreads at the top. Cyclonic or Frontal rain: This type of rainfall occurs when warm and cold air meets each other. Since warm air is lighter, it rises above the cold air.
In this way,warm currents along the coast make the coastal areas warmer and cold currents make them cooler than usual. ... The parts of western Europe remains ice free during winter.
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Vertical rays heat up a smaller surface. ... Vertical rays travel through a shorter distance in the atmosphere and the loss of heat is less. Slanting rays travel a longer distance through the atmosphere where much of its heat is absorbed by clouds, water vapour and dust particles.
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Convectional rainfall: When the temperatures are high, the air gets heated. Warm air rises higher into the atmosphere; it then expands and spreads at the top. ... Cyclonic or Frontal rain: This type of rainfall occurs when warm and cold air meets each other. Since warm air is lighter, it rises above the cold air.