In India, the pre-monsoon season is marked by numerous thunderstorms and lightning incidents. Describe the formation of thunderstorms in this setting and talk about the effects of pre-monsoonal rainfall in different parts of India.
Short-distance winds known as "local winds" are brought on by the unequal heating of the land and water in a specific location. Local winds impact certain areas and are more transient than global winds, which travel around the earth. These winds have a significant impact on a location's daily enviroRead more
Short-distance winds known as “local winds” are brought on by the unequal heating of the land and water in a specific location. Local winds impact certain areas and are more transient than global winds, which travel around the earth. These winds have a significant impact on a location’s daily environment and weather. The sea breeze, which happens during the day, is one typical local wind type. The heated air above the land rises as the sun heats the land more quickly than the sea, and cooler air from the sea replaces it, producing a cool breeze. In contrast, a land breeze blows from the land to the sea at night.The mountain and valley breeze is another example; it is found in hilly or mountainous regions and is characterised by warm air rising from the valleys and moving up the slopes during the day and cooler air flowing down the mountains into the valleys at night. These winds can affect temperature and humidity, causing drought-like conditions in desert regions and lowering temperatures in coastal areas.
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A common feature of the weather during the pre-monsoon season, i.e., March, April and May, over the Indian region is the outburst of severe local convective storms which often turn into thunderstorm and lightning. The intense convection activity due to strong heating of land mass over Chhotanagpur pRead more
A common feature of the weather during the pre-monsoon season, i.e., March, April and May, over the Indian region is the outburst of severe local convective storms which often turn into thunderstorm and lightning. The intense convection activity due to strong heating of land mass over Chhotanagpur plateau and movements towards southeast and mixing with warm air mass triggers the Nor Westers to develop which is locally named as Kal-Baisakhi (Bengal region) and Bardoli Cheerha (Assam). Apart from this, Mango Showers or Blossom Showers in Kerala and coastal Karnataka regions are some famous local storms of pre-monsoon season in India. Thunderstorms are characterized by towering cloud masses (mostly Cumulonimbus) with sudden electrical discharges manifested by a lightning and thunder enjoined with vigorous circulations and thus has the potential to spawn severe weather.
Formation of thunderstorms evolves in three stages
1.Cumulus Stage
2. Mature Stage
3.Dissipating Stage
Impact of pre-monsoonal rainfall
Pre-Monsoon storms mark the beginning of agricultural activities as it helps in ploughing and getting the field ready for the season. However, these storms are also associated with hailstorm and high speed winds of short duration, which are harmful for crops like mango and other standing crops.
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