• साइबेरियन उच्चदाब | |
siberian: साइबेरियाई | |
high: प्रखर स्वर्ग भारी | |
siberian high मीनिंग इन हिंदी
siberian high उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- Winters are dry due to the influence of the Siberian high-pressure system.
- They are cold and dry continental air of temperate latitudes of the Siberian High.
- During India'Us winter, however, the expansive Siberian high dominates, promoting dry northerly winds that shut off precipitation.
- Arctic high-pressure systems such as the Siberian High are cold core, meaning that they weaken with height.
- In winter, the Siberian High develops over the Eurasian land mass and the Aleutian Low develops over the northern Pacific Ocean.
- This is because of the influence of the East Asian monsoon in summer and the bitterly cold Siberian High in winter.
- The area experiences a subarctic climate, with the Siberian High resulting in very low temperatures and precipitation from November to March.
- In the winter, southern Siberia sits near the center of the semi-permanent Siberian High, so winds are usually light in the winter.
- For example, the Beaufort High an extension of the Siberian High system is a pressure system that drives the anticyclonic motion of the Beaufort Gyre.
- In winter the city is topographically influenced by expanding Siberian High-pressure zones and prevailing west winds, temperatures dropping as low as-20 �C (-4 �F ).