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A glacier is a huge mass of ice that moves slowly over land. The term “glacier” comes from the French word glace (glah-SAY), which means ice.
- Mountain glaciers
- Valley glaciers.
- Tidewater glaciers.
- Piedmont glaciers
- Hanging glaciers.
- Cirque glaciers.
- Ice Aprons.
- Rock Glaciers.
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Yogita Ingle 7 years ago
Dew: When the moisture is deposited in the form of water droplets on cooler surfaces of solid objects such as stones, grass blades and plant leaves, it is known as dew. The ideal conditions for its formation are clear sky and calm air, high relative humidity and cold and long nights. It is also necessary that the dew point is above freezing point.
Frost: When the dew point is below freezing point the water vapour will accumulate on the earth’s surface in the form of small white ice particles. The formation of the ice particles over a large area is called frost. The frost is formed when the temperature of the air falls rapidly so that the water vapour present in the air is directly turned into solid particles without turning into liquid state.
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Yogita Ingle 7 years ago
The average temperature of the earth remains rather constant. It has been possible because whatever the amount of heat the earth receives from the sun in the form of short-waves, it radiates back to the atmosphere in the form of long waves. There exists a stage of heat balance or equilibrium between the earth and its atmosphere. This balance of heat is termed as the earth's heat budget.
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Yogita Ingle 7 years ago
The monsoons strangely affect the climate of India. To understand the mechanism of the Indian monsoon, it is first important to understand the few facts.
The Indian monsoon is characterized by the following three dominant factors :
(i) Seasonal reversal of direction in wind system. The monsoon winds blow from land to sea in winter and from sea to land in summer.
(ii) Seasonal heavy rainfall and drought are common features of the Indian monsoon.
(iii) In spite of local variations in climatic conditions, it unites the whole country in a single climatic thread of monsoon type of climate.
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