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ftciteseerx:oai:CiteSeerX.psu:10.1.1.539.9741
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openpolar
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.539.9741 2023-05-15T17:57:32+02:00 Originally published at: The Pennsylvania State University CiteSeerX Archives 2008 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.9741 en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.9741 Metadata may be used without restrictions as long as the oai identifier remains attached to it. https://www.zora.uzh.ch/7031/2/Delaloye_Perruchoud_Recent_Interannual_2008V.pdf text 2008 ftciteseerx 2016-01-08T10:59:12Z Recent interannual variations of rock glacier creep in the European Alps Recent interannual variations of rock glacier surface motion are compared for 16 landforms monitored for a few years in various parts of the European Alps. Large fluctuations have been observed particularly since 2002. Most investigated rock glaciers have shown a similar behavior whatever their location in the Alpine arc, their size, or their velocity. The observed interannual variations appear to be primarily related to external climatic factors rather than to internal characteristics. They are mostly well correlated with mean annual ground surface temperature shifts with a delay of a few months, reflecting the thermal wave propagation deeper into permafrost. Seasonal factors may also play a significant role: Text permafrost Unknown
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Open Polar
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Unknown
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ftciteseerx
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English
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| description |
Recent interannual variations of rock glacier creep in the European Alps Recent interannual variations of rock glacier surface motion are compared for 16 landforms monitored for a few years in various parts of the European Alps. Large fluctuations have been observed particularly since 2002. Most investigated rock glaciers have shown a similar behavior whatever their location in the Alpine arc, their size, or their velocity. The observed interannual variations appear to be primarily related to external climatic factors rather than to internal characteristics. They are mostly well correlated with mean annual ground surface temperature shifts with a delay of a few months, reflecting the thermal wave propagation deeper into permafrost. Seasonal factors may also play a significant role:
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The Pennsylvania State University CiteSeerX Archives
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| format |
Text
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| title |
Originally published at:
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Originally published at:
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Originally published at:
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originally published at:
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| publishDate |
2008
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| url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.9741
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| genre |
permafrost
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| genre_facet |
permafrost
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| op_source |
https://www.zora.uzh.ch/7031/2/Delaloye_Perruchoud_Recent_Interannual_2008V.pdf
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| op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.539.9741
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| op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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1766165994475094016
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