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Indian Climate
Vegetation And Wildlife
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- Before studying Indian Climate, Vegetation and Wildlife, we must understand why natural transformation takes place on Earth.
- The Earth revolves around the Sun, and its axis is tilted at an average 23½°. Because of this revolution and axial tilt, different parts of the Earth receive different amounts of sunlight during different times of the year.
- This creates variation in temperature over time.
- This temperature variation is the basic reason behind the change of seasons, climate, vegetation and wildlife.
- So, the foundation of this chapter is: Revolution of Earth + Axial Inclination = Temporal Variation in Temperature = Seasonal and Climatic Transformation.
- Now, with this understanding, we will study the chapter Indian Climate, Vegetation and Wildlife.
Atmosphere
- The blended mixture of gases that surrounds the Earth is known as the atmosphere.
Weather
- The day-to-day transforming atmospheric condition is known as weather.
Climate
- For a long period, for near about 30 +- years, the ideal /static weather condition that persists for a particular place is known as the climate of that place.
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Season
- A particular and, on average, certain period of the year when it has a distinguished, specialised climatic feature-driven condition year on year, known as a season.
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Seasons
of India
Season
according to "Bharat Ritu Panchang"
Summer
season
- Sunrays are vertical in India, causing high temperatures all over India.
- The average temperature is high, causing the hot climatic conditions starting from March 1st to the 15th of June.
Winter
season
- In general, sunrays are slanting in India, which are extreme in North India, causing much cold in North India and moderate temperatures in South India.
- Due to this incoming of winter in trpical is late which is almost negligible in Tamil Nadu, Kerala, and South India
- The average temperature is very low in North India, causing a cold climatic condition from December to February.
Loo
- It is an example of a wind.
- The wind, which is very hot in temperature and blows over the high-temperature zone of the Indian subcontinent-
01- North India,
02- Pakistan and
03- Bangladesh.
Southwest
monsoon
- Another example of wind.
- As we know, wind blows from a high-pressure (P+) towards the low-pressure (P-).
- Starting from April, a low-pressure belt -ITCZ-starts to shift towards India from the Indian Ocean, encircling a complete circle around June onward over India, causing the rainy season known as the "Southwest monsoon".
Autumn
- The monsoon retrieval is the shifting of the low-pressure belt -ITCZ- from India towards the south, over the Indian Ocean towards the equator, known as the autumn season.
- By observing the above image, we can easily understand that it is the time of the "Autumn Equinox".
- What is the Equinox? We have studied in the previous chapters.
Affecting
factors of climate
- Altitude,
- location of a particular place,
- distance from the sea and
- The relief feature of a place determines the climatic condition.
Regional
differences
- All over India, due to a wide range of geographical variations, we experience climatic regional differences.
- That is because a particular geographical region has a distinct climatic condition from the surrounding or nearby different climatic regions.
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Moderate
climate
- A moderate climate means a place having an accommodating type of climatic condition where climatic transformations are almost negligible.
- For example, in the summer season, we continuously experience the summer despite the day-to-day temperature fluctuation conditions or having pre-monsoon showers.
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Mawsynram
- A region in the state of Meghalaya records the highest rainfall worldwide.
Vegetation
and Natural vegetation
- Plants,
- Shrubs,
- Grasses are the product of the inter-relationship between physical, climatic, and geological factors.
- Physical,
- Climatic, and
- Geology factors.
That patch of vegetation that grows and develops naturally, that is, without anthropogenic interference, is known as natural vegetation.
Important/decisive
factor of the character of the vegetation
- Temperature -&-
- precipitation of a particular place.
Tropical
vegetation and evergreen Forest
- which has a yearly rainfall of more than 200 cm, is known as tropical vegetation.
- This vegetation grows in the torrid zone / Tropical Zone / 20 Degree N/S latitudes, in general, on the Earth.
- In a very specific latitudinal extension, the highest density of this vegetation is found between 10 degrees north and 10 degrees south latitude.
- Because in the torrid zone, we don't have a season, that's why the tree sheds its leaves according to its convenience, and not according to season.
- That's why all around the year, vegetation looks green; the result is known as evergreen vegetation.
Tropical
deciduous forest -&- Monsoon forest
- That vegetation has an annual precipitation of 50 cm to 100+ cm.
- This vegetation sheds its leaves in the spring season.
- The majority of vegetation in India is Tropical deciduous.
Thorny
bushes
- This vegetation receives annual rainfall between 25 and 50 centimetres.
- Found in the region of western Rajasthan & in the Deccan Plateau.
Mountain
vegetation
- The mountain vegetation categorisation is based on the altitude.
- With increasing and decreasing attitudes, the character of the vegetation also transforms.
- Found over the Himalayas, the Western Ghats, Nilgiri and Anaimalai hills.
Coniferous
trees
- The mountain vegetation between the heights of 1500 and 2500 m is commonly known as coniferous trees.
- Found over the Himalayas region specifically.
Natural habitat?
- A place where living beings used to live in a natural environment, known as a natural habitat.
Migratory
Birds?
- When birds change their locations to a new location that has a more accommodating environment due to the transformation in seasons known as migratory birds.
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