The Earth from the Air: Yann Arthus-Bertrand

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The Earth from the Air: Yann Arthus-Bertrand

The Earth from the Air: Yann Arthus-Bertrand

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Price: £24.975
£24.975 FREE Shipping

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Although variations do occur, the temperature usually declines with increasing altitude in the troposphere because the troposphere is mostly heated through energy transfer from the surface. Main article: Troposphere A picture of Earth's troposphere with its different cloud types of low to high altitudes casting shadows. Next the mesosphere (pink) and the pink line of airglow of the lower thermosphere (dark), which hosts green and red aurorae over several hundred kilometers. In evaluating recent developments this revised edition reveals the earth’s fragility and the impact of humanity, but most of all the beauty of the natural world.

This is because the distance that particles can move without colliding with one another is large compared with the size of motions that cause mixing. Seeing (and photographing) the Earth from the sky allows a whole new perspective, as photographer Yann Arthus-Bertrand's diverse and colourful photographs demonstrate, from climbers on Mont Blanc to the winding rivers of Mongolia. The atoms and molecules are so far apart that they can travel hundreds of kilometres without colliding with one another. mi; 39,000 ft) above Earth's surface to the stratopause at an altitude of about 50 to 55 km (31 to 34 mi; 164,000 to 180,000 ft). It extends from the mesopause (which separates it from the mesosphere) at an altitude of about 80 km (50 mi; 260,000 ft) up to the thermopause at an altitude range of 500–1000 km (310–620 mi; 1,600,000–3,300,000 ft).Physical properties Comparison of the 1962 US Standard Atmosphere graph of geometric altitude against air density, pressure, the speed of sound and temperature with approximate altitudes of various objects.

ISBN 0-387-98746-0 , which rounds N 2 and O 2 to four significant digits without affecting the total because 0. The geological record however shows a continuous relatively warm surface during the complete early temperature record of Earth – with the exception of one cold glacial phase about 2. Sue B and Charlie W were on hand to offer advice/educate; the venue was excellent and the number of participants was about right to allow everyone to get attention. Much on show is conventional, exceptional landscape photography, but Arthus-Bertrand also trains his lens on our fingerprints smudging the idyll, such as the depressingly overcrowded shanty towns favelas of Rio de Janeiro or the sprawling communal rubbish heap of Mexico City.He is especially well known for his book The Earth from the Air , which has sold millions of copies since its first publication in 1999. Access Codes: Unless the book is described as "New," please assume that the book does *not* have an access code. He is especially well known for his book The Earth from the Air, which has sold millions of copies since its first publication in 1999.

This updated edition of the internationally acclaimed original features an updated text and over 100 breathtaking new photographs. Outgassing from volcanism, supplemented by gases produced during the late heavy bombardment of Earth by huge asteroids, produced the next atmosphere, consisting largely of nitrogen plus carbon dioxide and inert gases.Blue light is scattered more than other wavelengths by the gases in the atmosphere, surrounding Earth in a visibly blue layer at the stratosphere, above the clouds of the troposphere, when seen from space on board the ISS at an altitude of 335 km (208 mi) (the Moon is visible as a crescent in the far background). Temperature decreases with altitude starting at sea level, but variations in this trend begin above 11 km, where the temperature stabilizes over a large vertical distance through the rest of the troposphere. The surface-based homosphere includes the troposphere, stratosphere, mesosphere, and the lowest part of the thermosphere, where the chemical composition of the atmosphere does not depend on molecular weight because the gases are mixed by turbulence. The troposphere is bounded above by the tropopause, a boundary marked in most places by a temperature inversion (i.



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