The Zonally Symmetric Motion of the Atmosphere
The Zonally Symmetric Motion of the Atmosphere
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In our eReader you can find the full English version of the book. Read The Zonally Symmetric Motion of the Atmosphere Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Zonally Symmetric Motion of the Atmosphere
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Introduction When viewed from outer space, the earth's atmosphere, as evidenced by the cloud patterns, shows no signs of symmetry or regularityo However, analysis of wind and temperature data over long periods of time shows that on the average the atmosphere behaves in a regular manner. Prevailing westerlies, trade winds and the Hadley circulation are gross features of the motion which are observed from average data. In 1735j George Hadley initiated the idea that solar heating at the equator fo...rced the air there to rise, and hence he conjectured that the air, once aloft, travelled to the poles, where it sank back to the surface to journey toward the equator again. Subsequent observations by Ferrel around the 1880' s suggested that the air rising at the equator did not travel to the poles, but sank back to the surface at about 30 north or south latitude. In addition, the cold air sinking at the poles rose again at about 6o north or south latitude. In between these cells was a single cell rising at 6o and sinking at 30 in each hemisphere.
What to read after The Zonally Symmetric Motion of the Atmosphere?
You can find similar books in the "Read Also" column, or choose other free books by Donald a Drew to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Introduction When viewed from outer space, the earth's atmosphere, as evidenced by the cloud patterns, shows no signs of symmetry or regularityo However, analysis of wind and temperature data over long periods of time shows that on the average the atmosphere behaves in a regular manner. Prevailing westerlies, trade winds and the Hadley circulation are gross features of the motion which are observed from average data. In 1735j George Hadley initiated the idea that solar heating at the equator fo...rced the air there to rise, and hence he conjectured that the air, once aloft, travelled to the poles, where it sank back to the surface to journey toward the equator again. Subsequent observations by Ferrel around the 1880' s suggested that the air rising at the equator did not travel to the poles, but sank back to the surface at about 30 north or south latitude. In addition, the cold air sinking at the poles rose again at about 6o north or south latitude. In between these cells was a single cell rising at 6o and sinking at 30 in each hemisphere.
What to read after The Zonally Symmetric Motion of the Atmosphere?
You can find similar books in the "Read Also" column, or choose other free books by Donald a Drew to read onlineMoreLess
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