1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls

Permafrost degradation has been hypothesized as being one of the main causes of rockfalls and rockwall instability in the recent past in high mountain areas. Ongoing rockwall permafrost evolution remains poorly understood because of the lack of systematic measurements; models are often validated and...

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Main Authors: E. Cremonese, U. Morra Di Cella, S. Gruber, M. Giardino
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.439
http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.546.439 2023-05-15T17:56:48+02:00 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls E. Cremonese U. Morra Di Cella S. Gruber M. Giardino The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.439 http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.439 http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf Thermal diffusivity Rockwall temperature text ftciteseerx 2016-01-08T11:18:34Z Permafrost degradation has been hypothesized as being one of the main causes of rockfalls and rockwall instability in the recent past in high mountain areas. Ongoing rockwall permafrost evolution remains poorly understood because of the lack of systematic measurements; models are often validated and driven by few existing instrumented sites. In rockwall sub-surface temperature modelling, thermal diffusivity (κ) is one of the main parameters to be considered. In this study thermal diffusivity data series were inferred from rock temperature data in order to understand their annual variation, their distribution in different temperature ranges and their relation to atmospheric conditions. An harmonic analysis was performed to define amplitude and phase of the daily temperature waves at different depths by means of a least square minimizing optimization procedure. The analysis conducted shows that changes in κ values are influenced by different factors such as depth, season, rock temperature, aspect and snowfalls. Text permafrost Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Thermal diffusivity
Rockwall temperature
spellingShingle Thermal diffusivity
Rockwall temperature
E. Cremonese
U. Morra Di Cella
S. Gruber
M. Giardino
1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
topic_facet Thermal diffusivity
Rockwall temperature
description Permafrost degradation has been hypothesized as being one of the main causes of rockfalls and rockwall instability in the recent past in high mountain areas. Ongoing rockwall permafrost evolution remains poorly understood because of the lack of systematic measurements; models are often validated and driven by few existing instrumented sites. In rockwall sub-surface temperature modelling, thermal diffusivity (κ) is one of the main parameters to be considered. In this study thermal diffusivity data series were inferred from rock temperature data in order to understand their annual variation, their distribution in different temperature ranges and their relation to atmospheric conditions. An harmonic analysis was performed to define amplitude and phase of the daily temperature waves at different depths by means of a least square minimizing optimization procedure. The analysis conducted shows that changes in κ values are influenced by different factors such as depth, season, rock temperature, aspect and snowfalls.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author E. Cremonese
U. Morra Di Cella
S. Gruber
M. Giardino
author_facet E. Cremonese
U. Morra Di Cella
S. Gruber
M. Giardino
author_sort E. Cremonese
title 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
title_short 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
title_full 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
title_fullStr 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
title_full_unstemmed 1 Thermal Diffusivity Variability in Alpine Permafrost Rockwalls
title_sort 1 thermal diffusivity variability in alpine permafrost rockwalls
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.439
http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf
genre permafrost
genre_facet permafrost
op_source http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.439
http://app.fondazionemontagnasicura.org/multimedia/permadataroc/allegati/azione 4/nicop2008/pogliotti_et.al_thermal diffusivity variability in alpine permafrost rockwalls.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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