Hochschulschrift
Thermokarst and thermal erosion : degradation of Siberian ice-rich permafrost
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Dimensions
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30 cm
- Extent
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VI, 116 Bl.
- Language
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Englisch
- Notes
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Ill., graph. Darst., Kt.
Enth. 3 Sonderabdr. aus verschiedenen Zeitschr.
Potsdam, Univ., Diss., 2012 (Nicht für den Austausch)
- Keyword
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Dauerfrostboden
Sibirien
- Creator
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Morgenstern, Anne
- Table of contents
- Rights
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Bei diesem Objekt liegt nur das Inhaltsverzeichnis digital vor. Der Zugriff darauf ist unbeschränkt möglich.
- Last update
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11.03.2025, 11:39 AM CET
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Object type
- Hochschulschrift
Associated
- Morgenstern, Anne
Other Objects (12)
Thermokarst and thermal erosion : degradation of Siberian ice-rich permafrost
Organic Carbon Pools in Permafrost-Affected Soils of Siberian Arctic Regions
Organic carbon pools in permafrost-affected soils of Siberian Arctic regions
Gefrier- und Tauprozesse im sibirischen Permafrost : Untersuchungsmethoden und ökologische Bedeutung = Freeze and thaw in Siberian permafrost soils
Small-scale hydrological patterns in a Siberian permafrost ecosystem affected by drainage
Thermo-erosion of permafrost coasts in East Siberia
Microbial communities in submarine permafrost and their response to permafrost degradation and warming
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
Mass variations in the Siberian permafrost region based on new GRACE results and auxiliary modeling
How reliable is the mass variation in the Siberian permafrost region as observed by GRACE?
Content, distribution, and translocation of trace elements in permafrost-affected environments of the Siberian Arctic
Thermokarst and thermal erosion : degradation of Siberian ice-rich permafrost
Organic Carbon Pools in Permafrost-Affected Soils of Siberian Arctic Regions
Organic carbon pools in permafrost-affected soils of Siberian Arctic regions
Gefrier- und Tauprozesse im sibirischen Permafrost : Untersuchungsmethoden und ökologische Bedeutung = Freeze and thaw in Siberian permafrost soils
Small-scale hydrological patterns in a Siberian permafrost ecosystem affected by drainage
Thermo-erosion of permafrost coasts in East Siberia
Microbial communities in submarine permafrost and their response to permafrost degradation and warming
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
Mass variations in the Siberian permafrost region based on new GRACE results and auxiliary modeling
How reliable is the mass variation in the Siberian permafrost region as observed by GRACE?
Content, distribution, and translocation of trace elements in permafrost-affected environments of the Siberian Arctic
Thermokarst and thermal erosion : degradation of Siberian ice-rich permafrost
Organic Carbon Pools in Permafrost-Affected Soils of Siberian Arctic Regions
Organic carbon pools in permafrost-affected soils of Siberian Arctic regions
Gefrier- und Tauprozesse im sibirischen Permafrost : Untersuchungsmethoden und ökologische Bedeutung = Freeze and thaw in Siberian permafrost soils
Small-scale hydrological patterns in a Siberian permafrost ecosystem affected by drainage
Thermo-erosion of permafrost coasts in East Siberia
Microbial communities in submarine permafrost and their response to permafrost degradation and warming
Organic matter stored in ice-rich permafrost : future permafrost thaw and greenhouse gas release
Constraining mass variations in the Siberian permafrost region based on GRACE and Satellite Altimetry
Mass variations in the Siberian permafrost region based on new GRACE results and auxiliary modeling
How reliable is the mass variation in the Siberian permafrost region as observed by GRACE?