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Tropopause - Lambert M. Surhone
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Lambert M. Surhone:
Tropopause - Livres de poche

ISBN: 9786130322762

ID: 9786130322762

Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity 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. Tropopause: 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., Betascript Publishers

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Tropopause - Lambert M. Surhone
Livre non disponible
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Lambert M. Surhone:
Tropopause - Livres de poche

2009, ISBN: 6130322763

ID: 20025084104

[EAN: 9786130322762], Neubuch, [PU: Betascript Publishers Dez 2009], Neuware - 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. 72 pp. Englisch

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Tropopause - Lambert M. Surhone
Livre non disponible
(*)
Lambert M. Surhone:
Tropopause - Livres de poche

2009, ISBN: 6130322763

ID: 20025099864

[EAN: 9786130322762], Neubuch, [PU: Betascript Publishers Dez 2009], Neuware - 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. 72 pp. Englisch

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Agrios-Buch, Bergisch Gladbach, Germany [57449362] [Rating: 5 (von 5)]
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Tropopause - Lambert M. Surhone
Livre non disponible
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Lambert M. Surhone:
Tropopause - nouveau livre

ISBN: 9786130322762

ID: aca7c57db7a263c09ba52322988168f9

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. Bücher / Naturwissenschaften, Medizin, Informatik & Technik / Geowissenschaften

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Tropopause
Livre non disponible
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Tropopause - Livres de poche

2009, ISBN: 6130322763

Edition reliée, ID: 6031428

Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity - Buch, gebundene Ausgabe, 72 S., Beilagen: Paperback, Erschienen: 2009 Betascript Publishers

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Détails sur le livre
Tropopause: Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity

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.

Informations détaillées sur le livre - Tropopause: Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity


EAN (ISBN-13): 9786130322762
ISBN (ISBN-10): 6130322763
Version reliée
Livre de poche
Date de parution: 2009
Editeur: Betascript Publishers Dez 2009

Livre dans la base de données depuis 07.04.2008 21:55:22
Livre trouvé récemment le 04.11.2017 09:04:10
ISBN/EAN: 6130322763

ISBN - Autres types d'écriture:
613-0-32276-3, 978-613-0-32276-2


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