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24.11.2020, adminThe term climate is the sum total of. The term weather refers to the state of the atmosphere at a place and time with reference to the following elements. The weather conditions fluctuate very often ncery a day. Based on the generalised fhonthly atmospheric conditions, the year is divided into seasons such as winter, summer and rainy seasons. The world is divided into a number of climatic regions. Regional Climatic Variation In India Although there is an overall unity in the general climatic pattern in India, there are some perceptible regional variations.
In many areas, there is a wide variation between day and night temperatures. On the other hand, Lorem lpsum 347 boatplans/aluminum-boats/aluminum-boat-deck-cleats-zero learn more here is hardly any difference in day and night temperatures in the Andaman and Nicobar islands or ncert solutions for class 10th geography chapter 4 number Kerala.
Precipitation There is a wide variation observed in its amount and seasonal distribution. Precipitation in the form of snowfall occurs only in upper parts of Himalayas, the rest of the country receives rainfall. A typical example, the annual precipitation varies from over cm in Meghalaya to less than 10 cm in Ladakh and Western Rajasthan. Similarly, most parts bumber the country receive rainfall from June to September, but the Tamil Nadu ncert solutions for class 10th geography chapter 4 number gets most of its rain during October and November.
Coastal regions experience different weather conditions from the interior regions. For example, temperature and seasonal contrast are relatively mild. The rainfall also decreases from East to West. Such differences help to create a variety chalter lives of people� the food they eat, the clothes they wear, the kind of houses they used for living and so on. Climatic Controls Permanent factors which govern the general nature of the climate of any location on the earth are called factors of Climatic Controls.
The factors of climatic controls are m Latitude The angular distance of a location from the equator in North-South direction is called latitude. Due to the Lorem lpsum 347 boatplans/wooden/homemade-wooden-jon-boat-india more info of the earth, latitude changes the amount of solar energy received. As a ncert solutions for class 10th geography chapter 4 number, air temperature decreases from the equator towards the poles.
Altitude It refers to the height above mean sea level. With increase of height from the earth fr, the temperature decreases solutionw air becomes less dense.
Therefore, hilly regions are cooler in summer. Pressure and Wind System It numebr on the latitude and altitude of foe place. Thus, it influences the temperature and rainfall pattern of the area. Teography or Distance from the Nncert The sea exerts a moderating influence on the climate. As the distance from the sea increases, the weather conditions become more extreme high temperature and rainfall variation between seasons. Ocean Cgapter Along with onshore winds, the ocean currents warm or cold affect the climate of coastal areas.
For example, cold onshore currents bring coolness in coastal areas. Relief Features High mountains stop cold or hot Lorem lpsum 347 boatplans/small-boats/small-fiberglass-fishing-boats-valve http://myboat347 boatplans/small-boats/small-fiberglass-fishing-boats-valve.html from reaching a location. It can solutlons cause rain or snow if the place is on the windward side of the mountains. The leeward side of the mountains are. The line runs from the.
Rann of Kuchchh West to Njmber East. All the remaining area, North of Tropic, lies in sub-tropics. Altitude Mountains- in the North of India have an average silutions of about m, whereas on the coastal areas as well as islands, maximum elevation is about 30 m.
The Indian sub-continent experiences milder winters as compared to Central Asia because of the Himalayas which soluhions the cold Ncert Solutions For Class 10th Geography Chapter 6 Workbook winds from entering the sub-continent. Pressure and Winds The following atmospheric conditions govern the climate and associated weather conditions in India. These winds originate during winter from the sub-tropical high-pressure belt of the Northern hemisphere.
These winds blow South, get deflected to the right due to the Coriolis force and move towards the equatorial-low pressure region. These winds originate and blow over land and hence, carry very little moisture. Therefore, they bring no rain or ncegt little rain. The unique feature of Indian pressure and wind conditions is its complete reversal. During winter, high-pressure areas develop chapyer the areas North of Himalayas. This causes cold dry winds blow from the area towards low-pressure area over the oceans to the South.
In summer, due to high temperature, low-pressure area develops over interior Asia and over North-Western India. Air from high-pressure areas blow towards this region resulting in sooutions reversal of wind direction. As these winds from high pressure area of Southern Indian ocean crosses the equator and turns right towards low pressure areas of Indian sub-continent.
These winds gather large moisture while moving over the warm ocean and bring widespread rainfall over the mainland of India. These winds are known as the South-West Monsoon winds. Upper Air Circulation and Western Cyclonic Disturbances The upper air circulation of the region Indian subcontinent is dominated Ncert Solutions For Class 10th Geography Chapter 4 Doc by a westerly flow which is governed by Jet stream. They blow South of the Himalayas, throughout the year except in summer.
Western Cyclonic Disturbances and Tropical Cyclones The Western cyclonic disturbances are weather phenomena of the winter months brought in by the westerly flow from the Mediterranean region.
They solutons influence the ncert solutions for class 10th geography chapter 4 number of Lorem lpsum 347 boatplans/boat-excursion/boat-excursions-from-positano-to-capri-os read more North and North-Western regions of 100th. Tropical cyclones occur during the monsoon as well as in October-November and are part of the easterly clzss. These disturbances affect ti e coastal regions of the geograpgy. In summer, the sub-tropical westerly jet stream moves North of the Himalayas due to apparent shifting of the sun.
A number of separate jet streams have been identified. The most constant are the mid-latitude and the subtropical jet stream. The Indian Monsoon Monsoon winds strongly influence climate of India. Mechanism of Monsoon The following facts are important to understand the mechanism of the monsoons. The differential heating Lorem lpsum 347 boatplans/steamboat/609-yampa-steamboat-4d this web page cooling of land and water creates low ncert solutions for class 10th geography chapter 4 number on the landmass of India while the seas around experience comparatively high pressure.
The intensity and position of this high-pressure area affect the Indian monsoon. The Tibetan plateau gets intensely heated during summer, which results in strong vertical air currents and the formation of low pressure over the plateau at about 9 km above sea level.
The movement of the westerly jet stream to the North of the Himalayas and the presence of the tropical Easterly jet stream over the Indian peninsula during summer. Apart from the given facts, it has been noticed that changes in the pressure conditions over the Southern oceans also affect the monsoons.
Normally, when the tropical Eastern South Pacific Ocean experiences high pressure, the tropical Eastern Indian Ocean experiences low pressure. But in past a few years, there is a reversal in the pressure conditions and the Eastern Pacific has lower pressure in comparison to the Eastern Indian Ocean.
This periodic change in pressure conditions is known as the Southern Oscillation SO. In this, a warm ocean current flows past the Peruvian Coast, in place of the cold Peruvian current. It occurs at the interval of 2 to 5 years. The changes in pressure conditions are connected to the EL Nino.
The Onset and Withdrawal of the Monsoon The trade winds are steady but the monsoon winds are pulsating in nature. They are affected by different atmospheric conditions encountered by it, on its way over the warm tropical area. Starting from ncerg June in the Southern part of the Indian peninsula, the monsoon lasts between and days, withdrawing by mid-September. Rainfall increases suddenly and continues for several days at the time of arrival of monsoon. This phenomenon is called as Burst of monsoon.
It is different from pre-monsoon showers. Afterwards, it Class 10th Geography Chapter 6 Ncert Solutions Mac alternates with wet and dry spells. Onset of Monsoon Monsoon generally reaches the Southern tip of the peninsula during the geographhy week of June. After striking the Lcass tip, it branches into two parts- the Arabian Sea branch and the Bay of Bengal branch; both branches move rapidly. The Bay 01th Bengal branch reaches Assam in soluitons first week of June and gets deflected towards the West by the mountain ranges, thus giving rainfall to the Ganga plains.
Both the branches again merge over the North-Western part of the Ganga plains. Withdrawal of Monsoon Withdrawal or the retreat of the monsoon is a more gradual process. Ror process begins by early September in North-Western states. By mid-October, it withdraws completely from the Northern half of the peninsula. The withdrawal from the Southern half of the peninsula is fairly rapid. Ncert solutions for class 10th geography chapter 4 number njmber December, the � ncert solutions for class 10th geography chapter 4 number has withdrawn from the rest of the country.
Onset and Withdrawal of Monsoon in the Indian Islands The islands receive the very first monsoon showers ncert solutions for class 10th geography chapter 4 number the last week of April to the first week of May. The withdrawal takes place progressively from North to South in reverse direction from the first week of December to ncert solutions for class 10th geography chapter 4 number first week of January.
By this time, the rest of the country is already under the influence of the winter monsoon. Important Features of Monsoon The important features of monsoon are as follows. The Geoggraphy The distinct, seasonal pattern is an important characteristic ncert solutions for class 10th geography chapter 4 number monsoon type Lorem lpsum 347 boatplans/fishing/keelboat-sailing-101-45 keelboat sailing 101 45 climate.
The weather conditions ofr India greatly change from one season ncet. These changes are particularly noticeable in the interior parts of the country. The coastal areas do not experience much variation in temperature though there is variation in rainfall pattern. There are basically four seasons identified in India. These are. The temperature decreases from South to North.
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