Indian Climate and Monsoon Quiz

The type of climate found in India, characterized by distinct wet and dry seasons, heavily influenced by monsoon winds.

The Himalayan mountain range acts as a barrier to cold winds from the north, moderating temperature and influencing rainfall patterns.

The varied topography of India, including mountains, plateaus, and plains, creates diverse microclimates and impacts rainfall distribution.

Seasonal reversal of wind direction in India, bringing moisture-laden winds from the sea during the summer monsoon.

Uneven distribution of rainfall across India during the monsoon season, with some regions receiving significantly more rain than others.

The movement of moisture-laden winds from the Indian Ocean during summer, resulting in heavy rainfall across India.

The Malabar coast receives heavy rainfall in July due to the influence of the southwest monsoon, while the Tamil Nadu coast remains relatively dry.

The Northern Plains experience a continental climate characterized by hot summers and cold winters, due to its inland location and distance from the moderating influence of the sea.

Winter showers in Western Uttar Pradesh and Punjab are primarily caused by weak temperate cyclones originating from the Mediterranean Sea.

Kalbaisakhis are summer thunderstorms in West Bengal and Assam that significantly contribute to the growth of jute, rice, and tea.

The Himalayas block cold Siberian winds from reaching India, preventing it from becoming a cold desert.

The Himalayas force the South West Monsoon winds to rise, leading to heavy rainfall on the northern plains of India.

Thiruvananthapuram, located on the windward side of the Western Ghats, receives heavy rainfall from the South West Monsoon, while Chennai, on the leeward side, receives less rainfall from the weaker North East monsoon.

Cherrapunji, situated on the crest of the Khasi Hills, receives heavy rainfall due to its exposure to the South West Monsoon winds, while Shillong, on the upper (leeward) side, is in a rain shadow area and receives less rainfall.

Jaipur's location away from the sea and in the northern part of India results in a continental climate with a large temperature range, while Mumbai's coastal position leads to a more moderated climate.

The Himalayas are a major geographical feature that significantly influences India's climate, particularly the distribution of rainfall and temperature throughout the year.

The sudden and violent onset of rainfall in the first week of June, marking the beginning of the monsoon season.

A period of dryness during the monsoon season when rainfall ceases for two or more weeks.

Low-pressure systems originating in West Asia and the Mediterranean Sea that bring winter rain to the Indian plains and snowfall in the mountains.

Pre-monsoon showers in Karnataka, Kerala, Konkan, and Goa that aid in the ripening of mangoes.

Regions that receive minimal rainfall from the summer monsoon due to their geographical location.

Local winds that blow in India during the summer season.

The uneven distribution of monsoon rainfall across India is primarily due to relief rainfall, where windward sides receive more rainfall than leeward sides. Some places like the Aravali and Coromandel coasts, parallel to the southwest monsoon winds, receive little rainfall.

North India experiences extreme cold in winter due to its distance from the sea and the equator. This results in a continental type of climate with cold winters and hot summers.

Most of India remains dry during the northeast monsoon season because the northeast trade winds blow from land to sea, not carrying sufficient moisture for rainfall.

The period from October to November when the southwest monsoon winds weaken and retreat from North India.

The months of October and November, when retreating monsoon rain is experienced.

The northeast trade winds dominate during the winter season.

The northeast trade winds blow from land to sea, resulting in a dry climate for most parts of India. However, they contribute to some rainfall on the Coromandel coast, bringing cooler days and very cold nights.

The Himalayas protect the northern plains of India from the cold Siberian winds, preventing them from freezing in winter.

Rajasthan receives scanty rainfall due to its location in the rain shadow of the Aravali Mountains, which run parallel to the Arabian Sea branch, allowing winds to pass through without causing much rainfall.

Patna receives heavier rainfall than Delhi because it is located on the eastern side of the country, where rainfall is generally heavier.

Local hot winds bringing rainfall, crucial for mango ripening in Kerala.

Local winds in West Bengal during summer, bringing rainfall that benefits jute and rice crops.

Western Rajasthan doesn't get rain from the Arabian Sea branch of the South-West Monsoon because the winds blow parallel to the Aravali hills, not hitting them.

Mangalore's location on the Western Coast leads to moderate land and sea breezes throughout the year, keeping the temperature mild.

Shimla's higher altitude compared to Delhi means temperatures decrease, making it cooler in summer.

The Arabian Sea branch travels longer over the ocean, collecting more moisture, while the Bay of Bengal branch travels a shorter distance, carrying less moisture.

The Arabian Sea branch hits the Western Ghats directly, causing rainfall, while the Bay of Bengal branch travels further inland before hitting the mountains.

The eastern coast of Tamil Nadu and Andhra Pradesh receives rainfall from North-East Monsoon winds during January-February.

North East Trade winds cause the winter rain along the Coromandel Coast.

Tamil Nadu gets significant rainfall from the winter monsoon.

The Aravali range lies parallel to the moist winds from the Arabian Sea, not blocking them, preventing rain in Western Rajasthan.

Kochi's coastal location keeps it moderate, while Agra's distance from the sea causes extreme temperatures, leading to a high annual range.

Western disturbances entering from the Northwest bring winter cyclonic rain to the Northern plains and Punjab.

Tropical cyclones originate in the Bay of Bengal from local heat and moisture variations, while temperate cyclones originate in West Asia and the Mediterranean Sea.

The football match in Visakhapatnam was cancelled due to cyclones, triggered by the retreating monsoon and low pressure conditions over the Bay of Bengal.

Tamil Nadu gets rainfall from the retreating monsoon.

Meghalaya and Arunachal Pradesh receive over 200 cm of rainfall annually.

Kanyakumari's coastal location ensures a small difference between summer and winter temperatures, leading to an equable climate.

Chennai's lower latitude and proximity to the sea create a moderate climate, while Lucknow's inland location leads to extreme temperatures, resulting in a higher annual range for Lucknow.

Mangalore is on the windward side of the Western Ghats, receiving more rainfall than Mysore, which is on the leeward side.

The Tamil Nadu coast experiences dryness because it lies in the rain shadow of the Arabian Sea branch while the Malabar coast receives heavy rainfall due to the influence of the Bay of Bengal.

The Northern Plains experience extreme temperatures due to being far from the moderating influence of the sea, leading to hot summers and cold winters.

Central Maharashtra receives less rainfall than Western Maharashtra because it lies in the rain shadow region of the Western Ghats, while Western Maharashtra is on the windward side.

The annual rainfall for this station is 114.3 cm, calculated by adding up the rainfall for each month.

The station is likely located on the Coromandel Coast due to its moderate temperatures throughout the year and maximum rainfall during the winter season.

The season with the heaviest rainfall is the retreating monsoon, which occurs in September, October, and November.

The northern zone has cold winters and hot summers, while the southern zone is warmer with no clear-cut winter season.

The northern zone does not experience the sun directly overhead, whereas the southern zone experiences it at least twice a year.

Water bodies provide moisture for the summer monsoons, leading to heavy rainfall and moderate temperatures in coastal areas.

Jet streams are fast-moving, cold winds found in the upper layers of the atmosphere.

Jet streams influence India's climate by steering weather patterns, with the westerly jet stream prevalent during winter and the easterly jet stream guiding tropical depressions during the monsoon, impacting rainfall distribution.

India's climate varies due to diverse geographical features like mountains, deserts, oceans, and its vast latitudinal extent, leading to different climatic conditions in various regions.

Most of India receives rainfall from June to September due to the summer monsoon winds driven by differential heating of land and sea.

The South-West monsoon withdraws from northern India in October because the low pressure trough over the Ganga plains weakens due to the apparent southward movement of the sun, leading to high pressure and the end of the monsoon season.

El-Nino weakens the Indian monsoon due to increased sea surface temperatures, leading to drought-like conditions in the Indian sub-continent.

The North-East monsoon blows from December to February, originating from the landmass and moving towards the sea.

India's rainfall is characterized by a short, concentrated rainy season, accounting for 70% of the annual rainfall, primarily driven by relief-type rainfall where windward slopes receive more rain than leeward slopes.

Pune receives less rainfall than Mumbai because Mumbai is located on the windward side of the Western Ghats, while Pune is on the leeward side, resulting in less rainfall for Pune.

Tropical cyclones form due to low pressure over the sea, leading to high humidity and heavy rainfall. Temperate cyclones, with lower wind speeds and varying temperatures, bring light rainfall.

Kerala has a tropical climate due to its location near the equator, experiencing high temperatures and heavy rainfall. Punjab, located further north, has a continental climate with extreme temperature variations and less rainfall.