what are the reasons for development of thunderstorms in Hindi
Answers
Hello there,
एक तूफान एक बिजली और थंडर के साथ तूफान है।
गरज के साथ गरज के साथ गरज:
1) नमी: बादलों को बनाने और अंततः बारिश के लिए नमी की आवश्यकता होती है।
2) मोर्चा: समुद्र की हवा या पहाड़ों की तरह सामने जो गर्म हवा को ऊपर की ओर उठाने में मदद करते हैं।
3) तेजी से बढ़ती गर्म हवा: सूर्य की गर्मी के कारण, जगह का तापमान बढ़ जाता है।
तापमान में वृद्धि हवा को गर्म करती है और तेज हवाओं का निर्माण करती है जो ऊपर की दिशा में उठती है।
वज्रपात का कारण भारत जैसे गर्म और आर्द्र क्षेत्रों में आंधी-तूफान का विकास होता है।
बढ़ते तापमान से ऊपर की ओर तेज़ हवाएँ चलती हैं।
ये हवाएँ पानी की बूंदों को ऊपर की ओर ले जाती हैं जहाँ वे जम जाती हैं और फिर से गिर जाती हैं। बढ़ती हवा के साथ गिरती पानी की बूंदों की तेज गति बिजली और ध्वनि पैदा करती है।
यह एक वज्रपात है।
थंडरस्टॉर्म खतरनाक हैं।
बिजली गिरने से कई लोग मारे जाते हैं और जंगल और लंबे ढांचे को नुकसान होता है।
Hope you find my answer useful.
Harith
A thunderstorm, also known as an electrical storm or a lightning storm, is a storm characterized by the presence of lightning and its acoustic effect on the Earth's atmosphere, known as thunder.[1] Relatively weak thunderstorms are sometimes called thundershowers.[2] Thunderstorms occur in a type of cloud known as a cumulonimbus. They are usually accompanied by strong winds, heavy rain, and sometimes snow, sleet, hail, or, in contrast, no precipitation at all. Thunderstorms may line up in a series or become a rainband, known as a squall line. Strong or severe thunderstorms include some of the most dangerous weather phenomena, including large hail, strong winds, and tornadoes. Some of the most persistent severe thunderstorms, known as supercells, rotate as do cyclones. While most thunderstorms move with the mean wind flow through the layer of the troposphere that they occupy, vertical wind shear sometimes causes a deviation in their course at a right angle to the wind shear direction.
Thunderstorms result from the rapid upward movement of warm, moist air, sometimes along a front. As the warm, moist air moves upward, it cools, condenses, and forms a cumulonimbus cloud that can reach heights of over 20 kilometres (12 mi). As the rising air reaches its dew point temperature, water vapor condenses into water droplets or ice, reducing pressure locally within the thunderstorm cell. Any precipitation falls the long distance through the clouds towards the Earth's surface. As the droplets fall, they collide with other droplets and become larger. The falling droplets create a downdraft as it pulls cold air with it, and this cold air spreads out at the Earth's surface, occasionally causing strong winds that are commonly associated with thunderstorms.
There are four types of thunderstorms: single-cell, multi-cell cluster, multi-cell lines and supercells. Supercell thunderstorms are the strongest and most severe. Mesoscale convective systems formed by favorable vertical wind shear within the tropics and subtropics can be responsible for the development of hurricanes. Dry thunderstorms, with no precipitation, can cause the outbreak of wildfires from the heat generated from the cloud-to-ground lightning that accompanies them. Several means are used to study thunderstorms: weather radar, weather stations, and video photography. Past civilizations held various myths concerning thunderstorms and their development as late as the 18th century. Beyond the Earth's atmosphere, thunderstorms have also been observed on the planets of Jupiter, Saturn, Neptune, and, probably, Venus.
Stages of a thunderstorm's life.
Warm air has a lower density than cool air, so warmer air rises upwards and cooler air will settle at the bottom[4] (this effect can be seen with a hot air balloon).[5] Clouds form as relatively warmer air, carrying moisture, rises within cooler air. The moist air rises, and, as it does so, it cools and some of the water vapor in that rising air condenses.[6] When the moisture condenses, it releases energy known as latent heat of condensation, which allows the rising packet of air to cool less than the cooler surrounding air[7] continuing the cloud's ascension. If enough instability is present in the atmosphere, this process will continue long enough for cumulonimbus clouds to form and produce lightning and thunder. Meteorological indices such as convective available potential energy (CAPE) and the lifted index can be used to assist in determining potential upward vertical development of clouds.[8] Generally, thunderstorms require three conditions to form:
Developing stage
The first stage of a thunderstorm is the cumulus stage or developing stage. During this stage, masses of moisture are lifted upwards into the atmosphere. The trigger for this lift can be solar illumination, where the heating of the ground produces thermals, or where two winds converge forcing air upwards, or where winds blow over terrain of increasing elevation. The moisture carried upward cools into liquid drops of water due to lower temperatures at high altitude, which appear as cumulus clouds. As the water vapor condenses into liquid, latent heat is released, which warms the air, causing it to become less dense than the surrounding, drier air. The air tends to rise in an updraft through the process of convection (hence the term convective precipitation). This process creates a low-pressure zone within and beneath the forming thunderstorm. In a typical thunderstorm, approximately 500 million kilograms of water vapor are lifted into the Earth's atmosphere.