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Tropopause - Lambert M. Surhone
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Lambert M. Surhone:
Tropopause - Taschenbuch

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
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Lambert M. Surhone:
Tropopause - Taschenbuch

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
Vergriffenes Buch, derzeit bei uns nicht verfügbar.
(*)
Lambert M. Surhone:
Tropopause - Taschenbuch

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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Tropopause - Lambert M. Surhone
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Lambert M. Surhone:
Tropopause - neues Buch

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
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Tropopause - Taschenbuch

2009, ISBN: 6130322763

Gebundene Ausgabe, 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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Details zum Buch
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.

Detailangaben zum Buch - Tropopause: Earth's Atmosphere, Stratosphere, Lapse Rate, Equilibrium Level, Atmospheric Thermodynamics, World Meteorological Organization, Potential Vorticity


EAN (ISBN-13): 9786130322762
ISBN (ISBN-10): 6130322763
Gebundene Ausgabe
Taschenbuch
Erscheinungsjahr: 2009
Herausgeber: Betascript Publishers Dez 2009

Buch in der Datenbank seit 07.04.2008 21:55:22
Buch zuletzt gefunden am 04.11.2017 09:04:10
ISBN/EAN: 9786130322762

ISBN - alternative Schreibweisen:
613-0-32276-3, 978-613-0-32276-2


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