Summary

This document outlines the factors influencing monsoon patterns, including geographical considerations like latitude, altitude, and ocean currents. It describes different types of monsoons, emphasizing the impact of climate phenomena like La Niña and El Niño. The document also covers aspects of daily and annual weather patterns.

Full Transcript

# Monsoon ## India Retreating Monsoon A map of India showing the retreating monsoon. - It shows the dates on which the monsoon retreats from different parts of India. - It also shows various geographical features of India such as the Arabian Sea, Bay of Bengal, Lakshadweep, Andaman & Nicobar Is...

# Monsoon ## India Retreating Monsoon A map of India showing the retreating monsoon. - It shows the dates on which the monsoon retreats from different parts of India. - It also shows various geographical features of India such as the Arabian Sea, Bay of Bengal, Lakshadweep, Andaman & Nicobar Islands, and the Tropic of Cancer. - It also shows the bordering countries, such as Pakistan, China, Nepal, Bhutan, Bangladesh, and Myanmar. # Factors Affecting Climate of India - Latitude - Altitude - Pressure and Wind System - Relief Features - Ocean Currents - Distance from Sea # Climate The average weather in a given area over a longer period of time. Data taken of 30 years. # Weather The term refers to temporary conditions of the atmosphere, including temperature, atmospheric pressure, wind, humidity, precipitation, and cloud cover. ## Winter Season Chilling winds from the Arctic/Central Asia affects winter season, but they are blocked to a certain extent by the Himalayas. ### Winter Rainfall It is known as Upper Atmospheric Circulation. - At 25°N latitude in February, winds blow at 9-13 km height towards the east. - This is known as Jet Stream winds. - This wind carries Western Cyclonic Disturbances, which cause rainfall in the Northern Plains. - This is known as "Mahawat" in Rajasthan. - This is beneficial for Rabi crops. - Inward of Western Disturbances through Jet Streams is marked by increase in prevailing night temperature. ## Summer Season - In upper troposphere (9-13 km) very high speed of winds, there are Jet Streams that shift north and south as they follow boundaries of hot and cold air. - These Jet Streams blow west to east. - In the Indian Peninsula, summer rays fall over the Tibetan plateau, causing intense heating, which creates low pressure. - The low pressure causes trade winds to meet in the upper region, causing air to ascend, which results in rainfall. - This happens during July, between 20-25°N. # Pre-Monsoon Showers ## Nor-Westers - Also known as Kal Baisakhi - Calamity in the month of Baisakh in West Bengal. - Helpful for the growth of jute and tea. - In Assam, called Bardoli Chheerha. ## Blossom Showers - Seen in Kerala/Karnataka. - Helps in the growth and cultivation of coffee. ## Mango Showers - Seen in Kerala. - Helps in early ripening of mangoes. # On Set of Monsoon - It is derived from the Arabic word "Mausim,' which means seasonal reversal of winds. - It begins in Kerala in the first week of June in the Western Ghats. - This is known as Orographic rainfall. - Winds from the Southwest direction, which is why it is also known as the Southwest Monsoon. - This causes windward side (on shore side) and leeward side (off shore side) effect. # Rain Bearing System - The Bay of Bengal branch and Arabian Sea branch of the Southwest monsoon meet at Punjab. - Winds move parallel to Aravallis hence no rainfall in Rajasthan desert. - The North-Eastern Hills (Khasi Hills) receive the highest rainfall, with Mawsynram/Cherapunji being the wettest place on Earth. ## Break in Monsoon A sudden decrease in rainfall after the onset of the monsoon. ## Retreating Monsoon - Also known as North-East Monsoon. - It causes rainfall over the Coromandel coast (Tamil Nadu/Andhra). - Cyclonic disturbances occur in this region. ## In North India during this season - Clear skies - October heat (oppressing heat) # La Nina vs El Nino ## La Nina **Meaning:** Small Girl - Below average sea surface temperatures in east-central equatorial Pacific (cold phase on ENSO cycle). - Trade winds strengthen, pushing warm water westward. - Seen every 2- 7 years. - Leads to cooler global temperatures. - It can cause intense rainfall in Australia and India along with heavy floods; drier conditions in South America. - Fishing industries will flourish. ## El Nino **Meaning:** Child Christ/Small Boy - Above average sea temperatures in east-central equatorial Pacific (warm phase of ENSO cycle). - Trade winds weaken, allowing warm water to spread eastwards. - Seen every 3-7 years. - Leads to warmer global temperatures. - It can cause droughts in Asia and Australia and in the US, El Nino has its strongest impact during winter. - Fishing industries won’t flourish. # Variation in Temperature/Rainfall 1. Diurnal Range of Temperature (Daily range of temperature) 2. Annual Range of Temperature 3. Annual Range of Rainfall - Extremes of climate are seen in the interior of continents. - Coastal cities do not experience extreme climate due to "moderating influence of sea." - The further we go from ocean into the continent, the more is the extremity in the climate due to the continentality effect.. # Seasons and Months | Seasons | Months (According to the Indian Calendar) | Months (According to the Indian Calendar) | |--------------------------|-----------------------------------------------|------------------------------------------------| | Vasanta | Chaitra-Vaisakha | March-April | | Grishma | Jyaistha-Asadha | May-June | | Varsha | Sravana-Bhadra | July-August | | Sharada | Asvina-Kartika | September-October | | Hemanta | Margashirsa-Pausa | November-December | | Shishira | Magha-Phalguna | January-February |

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