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Tropopause
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H023H2IF7DV
Geliefert zwischen Mi., 22.04.2026 und Do., 23.04.2026
Details
High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! High Quality Content by WIKIPEDIA articles! The tropopause is the atmospheric boundary between the troposphere and the stratosphere. Going upward from the surface, it is the point where air ceases to cool with height, and becomes almost completely dry. More formally, it is the region of the atmosphere where the lapse rate changes from positive (in the troposphere) to negative (in the stratosphere). The troposphere is the lowest of the Earth's atmospheric layers and is the layer in which most weather occurs. The troposphere begins at ground level and ranges in height from an average of 11 km (6.8 miles/36,080 feet at the International Standard Atmosphere) at the poles to 17 km (11 miles/58,080 feet) at the equator. It is at its highest level over the equator and the lowest over the geographical north pole and south pole. On account of this, the coolest layer in the atmosphere lies at about 17 km over the equator. Due to the variation in starting height, the tropopause extremes are referred to as the equatorial tropopause and the polar tropopause.
Weitere Informationen
- Allgemeine Informationen
- GTIN 09786130322762
- Editor Lambert M. Surhone, Miriam T. Timpledon, Susan F. Marseken
- Sprache Englisch
- Genre Geowissenschaften
- Anzahl Seiten 72
- Größe H220mm x B150mm x T4mm
- Jahr 2009
- EAN 9786130322762
- Format Fachbuch
- ISBN 978-613-0-32276-2
- Titel Tropopause
- Untertitel Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity
- Gewicht 124g
- Herausgeber Betascript Publishers
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