climate class 9, climate class 9 in telugu, 9th social in telugu, ap dsc latest news, kings dsc

climate class 9, climate class 9 in telugu, 9th social in telugu, ap dsc latest news, kings dsc

#climate class 9 #climate class 9 in telugu #9th social in telugu #ap dsc latest news #kings dsc


హాయ్ నా పేరు సోమరాజు. ఏ పి డి ఎస్ సి కంటెంట్ ఎక్ష్ప్లైన్ చేయడానికి ఈ వీడియో లు చేస్తున్నాను. డి ఎస్సి ఖచ్చితంగా సాధించాలి అనేవారి కోసం ఈ వీడియోలు పక్కా ప్రణాళికతో తయారు చేయడం జరుగుతుంది. టెక్స్ట్ బుక్ నే ప్రామాణికం చేసుకొని ప్రతి పాయింట్ లైన్ టు లైన్ టచ్ చేసి అకాడెమి లెవెల్ లో ఒక్క పాయింట్ కుడా మిస్ కాకుండా ఈ వీడియో లు రూపొందించడం జరుగుతుంది. ఈ విడియోలు నచ్చితే లైక్ చేసి సబ్స్క్రయిబ్ చేసుకోండి. అనుదినము మీ ప్రిపరేషన్ లో నా వంతు సహాయంగా అందిస్తుంటాను.చుడండి టెక్స్ట్ బుక్ పాయింట్స్ ని సింపుల్ గా డివైడ్ చేసి మైండ్ మ్యాపింగ్ ద్వారా మీకు బోధించడం జరుగుతుంది. ఒక్కసారి ఈ విడియో చూస్తూ నోట్స్ ప్రిపేర చేసుకొని టెక్స్ట్ బుక్ టెక్స్ట్ బుక్ చుస్తే మికే అర్ధమౌతుంది యెంత పక్కాగా వుందో!


climate, conditions of the atmosphere at a particular location over a long period of time; it is the long-term summation of the atmospheric elements (and their variations) that, over short time periods, constitute weather. These elements are solar radiation, temperature, humidity, precipitation (type, frequency, and amount), atmospheric pressure, and wind (speed and direction).


From the ancient Greek origins of the word (klíma, “an inclination or slope”—e.g., of the Sun’s rays; a latitude zone of Earth; a clime) and from its earliest usage in English, climate has been understood to mean the atmospheric conditions that prevail in a given region or zone. In the older form, clime, it was sometimes taken to include all aspects of the environment, including the natural vegetation. The best modern definitions of climate regard it as constituting the total experience of weather and atmospheric behaviour over a number of years in a given region. Climate is not just the “average weather” (an obsolete, and always inadequate, definition). It should include not only the average values of the climatic elements that prevail at different times but also their extreme ranges and variability and the frequency of various occurrences. Just as one year differs from another, decades and centuries are found to differ from one another by a smaller, but sometimes significant, amount. Climate is therefore time-dependent, and climatic values or indexes should not be quoted without specifying what years they refer to.

Most surfaces are not perpendicular to the Sun, and the energy they receive depends on their solar elevation angle. (The maximum solar elevation is 90° for the overhead Sun.) This angle changes systematically with latitude, the time of year, and the time of day. The noontime elevation angle reaches a maximum at all latitudes north of the Tropic of Cancer (23.5° N) around June 22 and a minimum around December 22. South of the Tropic of Capricorn (23.5° S), the opposite holds true, and between the two tropics, the maximum elevation angle (90°) occurs twice a year. When the Sun has a lower elevation angle, the solar energy is less intense because it is spread out over a larger area. Variation of solar elevation is thus one of the main factors that accounts for the dependence of climatic regime on latitude. The other main factor is the length of daylight. For latitudes poleward of 66.5° N and S, the length of day ranges from zero (winter solstice) to 24 hours (summer solstice), whereas the Equator has a constant 12-hour day throughout the year. The seasonal range of temperature consequently decreases from high latitudes to the tropics, where it becomes less than the diurnal range of temperature.



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