• तापीय न्यून दाब • तापीय न्यूनदाब | |
thermal: गरम अंतःवस्त्र | |
low: निम्न होना रंभाहट | |
thermal low मीनिंग इन हिंदी
thermal low उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- 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.