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Rainfall

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Published in: Geography
17,250 Views

gives informational about rainfall ,types ,clouds etc.,

Acceleration T / Chennai

year of teaching experience

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  1. Rain fall
  2. Rain fall- formation diagram? Condosdion ours Air cols Sun heats grotd Råin Moist Land
  3. How rainfall Is formed? Sun heats UP water in lakes rivers or oceans and turns it in to water vapour or steam Water vapour goes UP in to the air Water vapour in the air gets cold and change back to liquid in to tiny drops of water, forming CIOUdS . OCCUrs when so much of water has condensed that the air cannot hold it any more.the CIOUdS get heavy and the water falls backs to the earth in the form of rain
  4. Types of rain fall Convectional rainfall Orographic rainfall Frontal rainfall
  5. Convectional rainfall Convective precipitation It results from heating of earth's surface that cause air to rise rapidly. As the air rises it cools and moisture condenses into clouds and PRECIPITATION. Conwc Oona' Precipitatio n Go oled Air Condense . Air "oiot par
  6. Orographic rainfall Prevailing winds Evaporation Orographic precipitation Warm ocean
  7. Oro graphic rainfall This kind of rainfall in mountainous regions is called orographic rainfall and it depends on slope lheight Itemperature and moisture content. This content of rainfall OCCUrs in the westernghats of india. Wind ward side receives heavy rain fall and the other side receives very little or no rain and is known as leeward side.
  8. Cyclonic rainfall Cyclonic or 'frontall rain OCCUrs where two air masses meet and form a 'front'. The warmer, moisture laden air rises over the colder air as a 'warm front'. As the air rises it cools, and its relative humidity increases. CIOUdS form as water vapour condenses, and then fall as rain.
  9. Cyclonic rainfall Frontal Rainfall warrm cold
  10. Highest rainfall TAJIK'S AFGHANISTAN/' PAKISTAN JAMMU KASHWR PRADESH PUNJ OELHi states in india INDIA State With Highest Rain Fall CHINA BHUTAN UTTAR PRADESH RAJASTHAN GUJARAT (ASSAM)/ MAFPUR ANGLADESÅAAV JHARKHAND MADHYA PRADESH (ODISHA} HÅVEI.' MAHARASHTRA MIZORAM ANMAR SAY BENGAL SEA RbjAfA State *ådeA' e.Gngeti•: W. ANDHRA PRAO€SH TAM'L 21+9-9 15616 CocntryCapital — 90'Hary State Map not to Scale Copyright e 2014 (Updated on 2nd June 2014) A SRI ANKA
  11. Clouds
  12. What Is CIOUdS? •A CIOUd is a large collection of very tiny droplets of water
  13. Classification of CIOUdS High CIOUdS(20/OOO feet (6/000 meters)) Middle CIOUdS (61500 to 20/000 feet (2/000 to 6/000 meters)) • Lower clouds(below 6/500 feet (2/000 meters)).
  14. High ,middle & lower clouds types High CIOUd types : include cirrus / cirrostratus and cirro CUmUIUS Middle CIOUdS types :alto stratus ,alto ClJmUIUS Low clouds types : strato ClJmlJIUS ,stratus nimbostratus ICUmUIUS ,cumulonimbus.
  15. Difference between sea and land breeze Warm Sea Breeze Ron,rn
  16. and Valley Breezes In areas where there are mountains and valleys we see a type of wind pattern known as mountain breezes and valley breezes. During the day, the surface of the mountain heats the air high up in the atmosphere, quicker than the valley floor can. As the warmer air expands a low pressure is created near the top of the mountain. This attracts the air from the valley, creating a breeze that blows from the valley floor up towards the top of the mountain. Often birds known as raptors, such as eagles, hawks, condors and vultures, float on these breezes to preserve their energy. This wind pattern is known as a valley breeze. In the evening, the mountain slopes cool the surrounding air more quickly than the air found lower in the atmosphere. This creates a high pressure as air becomes more densely packed. The resulting high pressure causes winds to blow down the mountain towards the valley floor. This type of wind pattern is known as a mountain breeze. Thus, in the daytime we typically see valley breezes as winds blow from the valley up towards the mountains. In the night we often see mountain breezes as winds travel from the mountains down towards the valleys.

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