(a) Kaal Baisakhi
(c) Trade Winds
(d) None of the above
(a) Cyclonic depression
(b) Retreating monsoon
(c) Western disturbances
(d) Southwest monsoon
(a) Early May
(b) Early July
(c) Early June
(d) Early August
(a) Warm days and warm nights
(b) Warm days and cold nights
(c) Cool days and cold nights
(d) Cold days and warm nightsAnswer :
(ii) (b) Loo
(iii) (c) Western disturbances
(iv) (c) Early June
(v) (b) Warm days and cold nights
Answer :There are six major controls of the climate of any place. They are:
Answer :India has monsoon type of climate because of strong influence of the monsoon winds. The summer monsoon causes heavy rainfall when they blow from sea to land. The winter monsoon winds blow from the interior of the continents to the sea and do not cause much rain. There is a seasonal reversal of the wind system 'monsoon'.
Answer :Thar Desert is the part of India that experiences the highest diurnal range of temperature. This is present towards western side of India in the state of Rajasthan. This is because it is filled with sand which gets heated up quickly during day and cooled up very quickly during nights. There is no sea closer to this area and hence there is no moderating effect.
Answer :South-West Monsoon Winds are responsible for rainfall along the Malabar coast.
Answer :Jet streams are high velocity westerly winds in the top most layer of the atmosphere. The westerly flows are responsible for the western disturbances experienced in the north and north-western parts of the country.
The movement of a jet stream affects temperatures and precipitation.
Answer :The seasonal reversal in wind direction during a year is called monsoon.
Break in monsoon is the absence of rains during the period of monsoon.
Answer :The monsoon is considered a unifying bond because: The Indian landscape, its flora and fauna, etc. are highly influenced by the monsoon. These monsoon winds bind the whole country by providing water for agricultural activities. Most of the festivals in India that are related to agricultural cycle may be known by different names in different parts of the country, but their celebration is decided by the monsoon. Year after year, people of India from north to south and from east to west, eagerly await the arrival of the monsoon. The river valleys which carry this water also unite as a single river valley unit.
Answer :The rainfall decreases from east to west in Northern India because the Bay of Bengal branch of Southwest monsoon moves towards north east carrying more moisture and they give heavy rainfall in this region. As they move further towards west, they carry less moisture content with themselves resulting in a decrease in rainfall in the west.
Answer :Seasonal reversal of wind direction over the Indian subcontinent takes place due to the differential heating and cooling of land and sea . This leads to the seasonal reversal of wind direction over the Indian subcontinent.
Answer :The monsoon begins from the first week of June and advances very rapidly to cover almost the whole country by mid- July. Hence, the bulk of rainfall in India is concentrated over a few months that is mainly from June to September.
Answer :The Tamil Nadu coast receives winter rainfall because of the movement of low-pressure condition to the Bay of Bengal. So, the veins now move from sea to land over Tamil Nadu.
Answer :This is due to the fact that the low-pressure condition over North Western India, which get transferred to the Bay of Bengal by early November. This shift is associated with the occurrence of cyclonic depression which originated in the history of the east coast of India.
Answer :It is because these places fall in the rain shadow region. Western parts of Rajasthan receive very low rainfall since Aravali Hills lie Parallel to monsoon winds. However, the leeward side of Western Ghats also experience very low rainfall because by the time the rain bearing winds move to this side, they are almost dry.
Answer :Despite an overall Unity in the general pattern there are susceptible regional variation in the climatic conditions within the country. For example
Answer :Cold Weather season begins from mid - November in Northern India and stays till February. December and January are the coldest month in the Northern parts of India. The northern parts of India experience high pressure and low temperature. However, Himalayas experience snowfall. A Characteristic feature of winter season is the western disturbances. These are the cyclonic disturbances which are brought to India by westerly jet stream and bring rainfall to Punjab and Haryana, snowfall to Jammu and Kashmir and Himachal Pradesh. This rainfall is very good for the Rabi crop wheat. The Peninsular India does not have a well-defined winter season. Tamil Nadu coast experiences winter rainfall.
(i) Areas receiving rainfall over 400 cm.
(ii) Areas receiving less than 20 cm of rainfall.
(iii) The direction of the south-west monsoon over India.Answers :
(I) Blue region shows the area receiving rainfall over 400 cm.
(ii) Green region the areas receiving less than 20 cm of rainfall.
(iii) Arrows shows the direction of the south-west monsoon over India.
Answers : Thiruvananthapuram (closest) → Bengaluru → Chennai → Mumbai → Nagpur → Kolkata → Shillong → Jodhpur → Delhi → Leh (farthest).
Answers : Kolkata (lowest) → Chennai → Mumbai → Thiruvananthapuram → Delhi → jodhpur → Nagpur → Bengaluru → Shillong → Leh (highest).
Answers :Mumbai and Shillong.
Answers :Leh and Jodhpur.
Answers :Chennai and Thiruvananthapuram
Answers :Leh (Coldest) and Jodhpur( Hottest).
Answers :Mumbai and Thiruvananthapuram
Answers :Shillong and Kolkata
Answers :Delhi and Kolkata
Answers :Chennai and Bengaluru
Answers :Jodhpur and Delhi
(a) February- Thiruvananthapuram and Chennai
(b) April- Nagpur and Chennai
(c) May – Nagpur, Jodhpur and Delhi
(d) June- Jodhpur and Delhi
Answer :The south-west monsoons hit Thiruvananthapuram and Shillong around the first of June. Thiruvananthapuram receives rain from the Arabian Sea branch while Shillong receives rain from the Bay of Bengal branch. After causing rains in these regions, the Arabian Sea Branch moves from south-west to north-east, while the Bay of Bengal branch moves from north-east to north-west. As a result, these regions receive lesser rainfall in the months succeeding June.
Answer :The Arabian Sea branch of the south-west monsoons reaches Thiruvananthapuram around the first of June. It reaches Mumbai around the tenth of June. So, Thiruvananthapuram receives much of its rainfall in the month of June, while Mumbai receives much of its rainfall in the month of July.
Answer :Chennai is situated on the Western Ghats, and is far away from the western coast. The Arabian Sea branch causes greater rainfall on the western coastline, while the eastern branch passes over Bay of Bengal, on to the north-eastern part of the country. As a result, Chennai gets low rainfall from the south-west monsoons.
Answer :Shillong is surrounded by hills and mountains, which causes the Bay of Bengal branch of the south-west monsoons to accumulate in this region. This is the reason why this region experiences heavy rainfall. On the other hand, Kolkata does not lie in a hilly area. Thus, it receives lesser rainfall as compared to Shillong.
Answer :The Bay of Bengal branch of the south-west monsoons reaches Shillong around the first of June. It gradually progresses from east to west. As a result, the amount of rainfall received by this region decreases from June to July. The monsoon winds reach Kolkata later than they arrive in Shillong. Hence, Kolkata receives more rainfall in July.
Answer :Due to the decrease in the humidity of the monsoon winds, the amount of rainfall decreases from east to west in northern India. Delhi lies to the east of Jodhpur therefore it receives more rain.
Answer :Thiruvananthapuram has an equable climate because of it is located near the sea. The sea exerts a moderating influence on the climate of the region.
Answer :Chennai experiences a lot of rainfall after the fury of monsoon is over in most parts of the country because of the retreating monsoons, and also because of the tropical cyclones.
Answer :Jodhpur lies in the north-western part of the country. The Great Indian Desert is located in this region. Due to the presence of sand, the region experiences high diurnal range of temperature. Hence, Jodhpur has a hot desert type of climate.
Answer :Leh experience snowfall due to the extremely low temperatures. As a result, it experiences moderate precipitation almost throughout the year.
Answer :Delhi and Jodhpur receive rainfall mostly from the south-west monsoons. Hence, the rains in these regions are confined to the monsoon period. While Thiruvananthapuram and Shillong receive heavy rains during the monsoons, their proximity to the sea makes them experience rains apart from the ones received during the monsoon period.
Answer :factors like wind systems, pressure, latitude, altitude, distance from the sea, presence of mountains, etc., are responsible for the presence of variations across the country, the seasonal arrival and retreat of monsoons provides a kind of climatic unity to the entire country.
Answer :Most of the world's deserts are located in the western margins of continents in the subtropics because of the tropical easterly winds. The tropical easterly winds become dry by the time they reach the western margins of the continents and so they bring no rainfall. Thus, the region gets no moisture which causes dry conditions leading to formation of deserts.
Answer :Because Rajasthan receives less rainfall so these thick walls prevent the heat from entering into the houses while the flat roofs help to retain the little water that has been collected during rainfall.
Answer :Because they are the region of heavy rainfalls therefore the sloping roofs helps them to get rid of the collected rainwater which flows down from the roof to the ground.
Answer :Houses in Assam are built on stilts or above the ground level to avoid flooding of houses due to heavy rainfall.
Answer :Chennai- rainy season, Mumbai- rainy season, Kashmir-winter, Delhi-summer, Srinagar- winter, Amritsar- winter, Shimla- winter.
Answer :In Chennai, much of the fury was unleashed by the Adyar river. As water from the Chembarambakkam reservoir was released into the river, whose depth and width had shrunk due to rapid urbanization and encroachments, it disgorged water into the neighborhoods along the banks.
In Mumbai, the thick slush-filled stench-emanating rivulet, the Mithi, which stretches from Powai Lake in the eastern suburbs to the Mahim Creek in the western part, was once a river that flowed out into the Arabian Sea. Like Adyar, Mithi too was lined with encroachments.
Owing to massive concretization of roads and unplanned constructions that have flattened the natural topography, almost 90 to 100 per cent of the rainwater in both cities drains off into the stormwater drains instead of being absorbed into the ground.
The Indian state of Kerala receives some of India’s highest rainfall during the monsoon season. However, during 2018 the state experienced its highest level of monsoon rainfall in decades. According to the India Meteorological Department (IMD), there was 2346.3 mm of rainfall, instead of the average 1649.55 mm.
Kerala received over two and a half times more rainfall over the average for August. Between August 1 and 19, the state received 758.6 mm of rainfall, compared to the average of 287.6 mm, or 164% more. This was 42% more than during the entire monsoon season.
In some areas, floodwater was between 3-4.5m deep. Floods in the southern Indian state of Kerala killed more than 410 people since June 2018 in what local officials said was the worst flooding in 100 years. Many of those who died had been crushed under debris caused by landslides. More than 1 million people were left homeless in the 3,200 emergency relief camps set up in the area.
Parts of Kerala’s commercial capital, Cochin, were underwater, snarling up roads and leaving railways across the state impassable. The state’s airport, which is used by domestic and overseas tourists, was closed, causing major disruption.
Local plantations were inundated by water, endangering the local rubber, tea, coffee and spice industries.
Schools in all 14 districts of Kerala were closed, and some districts have banned tourists because of safety concerns.
Maintaining sanitation and preventing disease in relief camps housing more than 800,000 people was a significant challenge. Authorities also had to restore regular supplies of clean drinking water and electricity to the state’s 33 million residents.