thermal low sentence in Hindi
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- Large-scale thermal lows over continents help drive monsoon circulations.
- Thermal lows tend to have weak circulations, and can extend to in height.
- Large-scale thermal lows over continents help create pressure gradients that drive monsoon circulations.
- Development of thermal lows inland of the coastline lead to the development of sea breezes.
- Highly elevated surfaces can induce a thermal low, which then augments the environmental wind flow.
- Within the tropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations.
- Thermal lows form due to localized heating caused by greater sunshine over deserts and other land masses.
- Without the thermal low pressure caused by the heating, there was no monsoon over the Indian subcontinent.
- The warmer air expands, becoming less dense than the surrounding air mass, and creating a thermal low.
- Elevated areas can enhance the strength of the thermal low as they warm more quickly than the atmosphere which surrounds them at the same altitude.
- The heating causes a thermal low to develop which sets up a pressure gradient which induces the wind, pulling cooler air down from the High Sierra.
- Thermal lows over the western and southern portions of North America, northern Africa, and southeast Asia are strong enough to lead to summer monsoon conditions.
- Because of this extreme heating process, a thermal low is usually noticed near the surface, and is the strongest and the most developed during the summertime.
- The monsoon circulation dominates across southern and eastern sections, due to the presence of the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.
- This is the case for Siberia were the temperature is very cold in winter forming the Siberian High, or very hot in summer to give a thermal low in summer.
- At the same time, the intense heating inland creates a pronounced thermal trough aligned with the Great Central Valley and typically linked to the broader thermal low across the North American deserts.
- The North American monsoon is associated with an area of high pressure called the subtropical ridge that moves northward during the summer months and a thermal low ( a trough of low pressure which develops from intense surface heating ) over the Mexican Plateau and the Desert Southwest of the United States.
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