INDIAN SEASONS - Geography - UPSCFEVER (2023)

Chapter 4: INDIAN SEASONS

Introduction

SEASONS IN INDIA

• Winter season, mid-December to mid-March




• Hot weather season, mid-March to May.




• Rainy season, June to September




• Season of retreating monsoon, October to mid-December.

There are three seasons in India:summer, winter and monsoon. The climate of India is essentially sub-tropical monsoonic. The word 'monsoon' has been derivedfrom the Arabic word "Mausim" which means 'season'. Originally, the word 'monsoon' was, usedby Arab navigators several centuries ago, to describe a system of seasonal reversal of winds alongthe shores of the Indian Ocean, especially over the Arabian Sea, in which the winds blow from thesouth-west to north-east during the summer season and from the north-east to south-west duringthe winter season.

Monsoon is a unique weatherphenomenon due to seasonal reversal of winds.

Features of Indian Monsoon

Monsoon has following features:

1.Suddenonset

2.Gradualadvance

3.Gradualretreat

4.Variation–temporal and regional

INDIAN MONSOON

• Monsoons are a complex meteorological phenomenon. Experts of meteorology have developeda number of concepts about the origin of monsoons. Some of the important concepts about theorigin of monsoons have been given as under




• The Thermal Concept of Halley :




• The primary cause of the annual cycle of the Indianmonsoon circulation was the differential heating effects of the land :and the sea.




• Monsoons are the extended land breeze and sea breezee on a large scale, produced by the differentialheating of continents and ocean basins. During the summer season in the Northern Hemisphere,when the Sun's rays are vertical over the Tropic of Cancer, the huge landmass of Asia heats quicklyand develops a strong low pressure centre near Lake Baikal (Siberia) and Peshawar (Pakistan).This thermal low extends up to 700 mb. Moreover, the pole-ward shift of the Inter-TropicalConvergence Zone (ITCZ) to a position over southern Asia reinforces the thermally induced lowpressure centre. In comparison to this, the pressure over the adjacent water of the Indian and thePacific Oceans is relatively high. Under these conditions, a sea-to-land pressure gradient develops.Consequently, the surface air flow is from the high pressure over the oceans towards the low pressureareas over the heated landmass. Under the extreme low pressure condition on land, the wind fromthe southern part of the Indian Ocean (south of Equator) is attracted towards the subcontinent of India.




• The air coming from oceans towards land is warm and moist. When land barriers like mountainranges and plateaus come in the way of the moisture-laden winds, they ascend and result intosaturation, condensation, and precipitation




• In the Northern Hemisphere during winter season, there develops high pressureareas near Baikal Lake (Siberia), and Peshawar {Pakistan}. As compared to these high pressures,the Indian Ocean and the Pacific Ocean (south of Japan) remain relatively warm, having low pressureareas.




• Consequently, there is an outflow of air from the high pressure of the land to the low pressureareas of the oceans. The air blowing from high pressure areas of land towards the sea is cold anddry. This cold and dry air is incapable of giving precipitation unless it comes into contact withsome water body (ocean/sea)




• Criticism of The Thermal Concept of Halley

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• The low pressure areas that develop over the continents during the summer season in theNorthern Hemisphere are not stationary. These low pressure areas change their position(location) suddenly, This sudden change in the low pressure areas are not exclusively relatedto low thermal conditions.




• Had the monsoon been thermally induced, there would be anti-monsoon circulation ill theupper air of the troposphere, which is lacking.




• Halley did not take into consideration the Coriolis effect of rotation of the earth on its axis.On a rotating earth, the wind has a tendency to move towards its right in the NorthernHemisphere and towards its left in the Southern Hemisphere.




• The role of latent beat passing into the atmosphere through water vapour was also notconsidered by Halley; water vapour also plays an important role in the origin and developmentof monsoons.




• The modern researches in meteorology have shown that the monsoon rainfall is not whollyorographic. They are an amalgamation of convectional, orographic and cyclonic rainfall.

Indian Monsoon

Stage 1:

The apparent movement of the sunin northern hemisphere in summer is seen. This heats the Tibetan plateau and theair rises upwards. This creates a Tropical Eastern Jetstreamwhich descends at Madagascar and creates a high pressure zonethere. An inter tropical convergence zone [ITCZ] formed atequator moves to Tibetan plateau.

Fig 1: Indian monsoon

Stage 2:

The Somali jet stream intensifiesthe Somalian ocean current during summer. Stronger the Somaliancurrent better the monsoon.

Stage 3:

Sub tropical westerly jetmaintains high pressure over North India. The STWJ is bifurcatedby the Himalayas into two branches.

Fig 2: STWJ and Himalayas

The summer see apparent movementof the sun and heating of the Tibetan plateau. This creates alow pressure belt over Tibet.

The STWJ still continues to beover South Himalayas and it resists the monsoon winds.

In this time there is localconvectional rainfall in Bengal, Bihar called Kalbaisakhi ,mango showers. These are pre monsoon thunder showers.

Then the STWJ southern branchmoves over north and STWJ withdraws from theIndian subcontinent. If this branch reestablishes then monsoonbreak is seen.

Stage 4: Indian OceanDipole

Low pressure conditions overAustralia and Tibetan plateau and high pressure over Madagascarcreate an Indian ocean dipole. A strong dipole pushes monsoonwinds towards Indian subcontinent.

Fig 3: Indian Ocean Dipole

Stage 5: onset ofmonsoon

The monsoon winds have twobranches Arabian and Bay of Bengal. The Arabian branch movesover western ghats and is blocked. This brings heavy rainfallover western region.

The SW Arabian branch isn'tblocked by Aravallis so less monsoon over Rajasthan. The gapbetween Vindhyas and Aravallis mean SW winds reach over toHimachal Pradesh.

The Eastern branch of the SWmonsoon goes over Bay of Bengal and isn't blocked by the easternghats. It passes through their gaps and reaches Vindhya ,Satpuda range and Chota Nagpur plateau. This gives rainfall tothe Eastern India and interiors.

The second part of the easternbranch of sw monsoon passes over north east and brings rainthere.

Stage 6: retreatmonsoon

The month of September the ITCZretreats towards the equator from Tibetan plateau. As it passesover the India the eastern branch of South west monsoon andnorth east winds collide.

The eastern branch of South west monsoonwithdraws first. Then North East winds are off land and hencedry but they pick moisture over Bay of Bengal and bring rain tosouthern tip of India i.e. Coast of Andhra Pradesh, Tamil Nadu.

The retreating eastern branch ofSouth west monsoon bringscyclones to the land.

Fluctuations in Indian monsoon:

1.If the Indian oceandipole is weak.

2.Southern oscillation isreversed or not strong.

3.SWTJdoesn’t retreat from India or comes back once again.

4.Inadequateheatingof Tibetan plateau.

Solved Question Papers

Q.With reference to ‘Indian Ocean Dipole (IOD)’ sometimes mentioned in the news while forecasting Indian monsoon, which of the following statements is/are correct?
1. IOD phenomenon is characterized by a difference in sea surface temperature between tropical Western Indian Ocean and tropical Eastern Pacific Ocean.
2. An IOD phenomenon can influence an El Nino’s impact on the monsoon.Select the correct answer using the code given below: (UPSC CSAT 2017)

1. 1 only




2. 2 only




3. Both 1 and 2




4. Neither 1 nor 2

Ans . B

1. Indian Ocean Dipole (IOD) is an event which the western Indian Ocean becomes alternately warmer and then colder than the eastern part of the Indian ocean.

2. A positive IOD leads to greater monsoon rainfall and more active (above normal rainfall) monsoon days while negative IOD leads to less rainfall and more monsoon break days

Q.Consider the following statements:
1. In India, the Himalayas are spread over five States only.
2. Western Ghats are spread over five States only.
3. Pulicat Lake is spread over two States only.
Which of the statements given above is/are correct? (UPSC CSAT 2017)

1. 1 and 2 only




2. 3 only




3. 2 and 3 only




4. 1 and 3 only

Ans . B

1. Western Ghats are spread over six States

Q.With reference to river Teesta, consider the following statements:
1. The source of river Teesta is the same as that of Brahmaputra but it flows through Sikkim.
2. River Rangeet originates in Sikkim and it is a tributary of river Teesta.
3. River Teesta flows into Bay of Bengal on the border of India and Bangladesh.
Which of the statements given above is/are correct? (UPSC CSAT 2017)

1. 1 and 3 only




2. 2 only




3. 2 and 3 only




4. 1, 2 and 3

Ans . B

1. Teesta merges into Brahmaputra itself rather than flowing into sea by its own

Q.If you travel by road from Kohima to Kottayam, what is the minimum number of States within India through which you can travel, including the origin and the destination? (UPSC CSAT 2017)

1. 6




2. 7




3. 8




4. 9

Ans . B

1. Nagaland, Kohima, Assam, W.Bengal, Odisha, Andhra Pradesh, Karnataka (or Tamilnadu), Kerala, Kottayam

Q.At one of the places in India, if you stand on the seashore and watch the sea, you will find that the sea water recedes from the shore line a few kilometres and comes back to the shore, twice a day, and you can actually walk on the sea floor when the water recedes. This unique phenomenon is seen at (UPSC CSAT 2017)

1. Bhavnagar




2. Bheemunipatnam

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3. Chandipur




4. Nagapattinam.

Ans . C

1. Chandipur beach has a unique distinction on its own. Unlike other beaches, the sea water here recedes away from the shore line about five km twice a day, an unusual phenomenon, rarely found anywhere.

Q.Which of the following is geographically closest to Great Nicobar ? (UPSC CSAT 2017)

1. Sumatra




2. Borneo




3. Java




4. Sri Lanka

Ans . A

1. Sumatra seems quite closer to Great Nicobar than Sri Lanka.

Q.Mediterranean Sea is a border of which of the following countries?
Jordan
Iraq
Lebanon
Syria
Select the correct answer using the code given below: (UPSC CSAT 2017)

1. 1, 2 and 3 only




2. 2 and 3 only




3. 3 and 4 only




4. 1, 3 and 4 only

Ans . C

1. Mediterranean Sea doesn’t touch Jordan and Iraq

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