walker circulation sentence in Hindi
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- Changes in the Walker circulation with time occur in conjunction with changes in surface temperature.
- These trade wind fluctuations can be understood as the weakening and strengthening of the Atlantic Walker circulation.
- The two phases relate to the Walker circulation, discovered by Gilbert Walker during the early twentieth century.
- In 1924, Gilbert Walker ( for whom the Walker circulation is named ) coined the term " Southern Oscillation ".
- An especially strong Walker circulation causes a " La Ni�a ", resulting in cooler ocean temperatures due to increased upwelling.
- A scientific study published in May 2006 in the journal Nature indicates that the Walker circulation has been slowing since the mid-19th Century.
- However, a new study from The Twentieth Century Reanalysis Project shows that the Walker circulation has not been slowing ( or increasing ) from 1871 2008.
- Crops that lie on the equatorial belt or under the tropical Walker circulation, such as rice, will be affected by varying monsoon patterns and more unpredictable weather.
- The Walker circulation & ndash; a broad atmospheric circulation & ndash; caused unusually moist conditions in the eastern Indian Ocean while producing an increase in subsequent season.
- The Walker circulation is caused by the pressure gradient force that results from a high pressure system over the eastern Pacific Ocean, and a low pressure system over Indonesia.
- The overall lack of activity was due to a strong Walker circulation over Indonesia, which increased convection over the Australian region, but suppressed convection over the Indian Ocean.
- During non-El Ni�o conditions, the Walker circulation is seen at the surface as easterly trade winds that move water and air warmed by the sun toward the west.
- The Walker circulations of the tropical Indian, Pacific, and Atlantic basins result in westerly surface winds in northern summer in the first basin and easterly winds in the second and third basins.
- Meanwhile, in the Atlantic, fast-blowing upper level Westerlies of the Hadley cell, which would ordinarily be blocked by the Walker circulation and unable to reach such intensities, form.
- There are projected increases of wind shear in the tropical Atlantic and East Pacific associated with the deceleration of the Walker circulation, as well as decreases of wind shear in the western and central Pacific.
- When the Walker circulation weakens or reverses, an " El Ni�o " results, causing the ocean surface to be warmer than average, as upwelling of cold water occurs less or not at all.
- Changes in ocean currents would also affect local sea levels, as is the case in the Pacific where the sea levels are around half a meter higher in the west than in the east due to the Walker circulation and cold Humboldt Current.
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