Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ...
Permafrost is a common characteristic of Arctic landscapes, where it refers to ground that remains at or below 0 °C for a duration of at least two consecutive years. Permafrost underlies approximately 15 % of the landmass in the Northern Hemisphere and is becoming more susceptible to rapid thawing a...
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ftdatacite:10.3929/ethz-b-000655439 2024-04-28T08:07:53+00:00 Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... Maier, Kathrin Bernhard, Philipp Hajnsek, Irena 2023 application/pdf https://dx.doi.org/10.3929/ethz-b-000655439 http://hdl.handle.net/20.500.11850/655439 en eng ETH Zurich Permafrost Retrogressive Thaw Slumps DEM infoeu-repo/classification/ddc/550 Earth sciences Conference Poster article-journal Text ScholarlyArticle 2023 ftdatacite https://doi.org/10.3929/ethz-b-000655439 2024-04-02T12:32:08Z Permafrost is a common characteristic of Arctic landscapes, where it refers to ground that remains at or below 0 °C for a duration of at least two consecutive years. Permafrost underlies approximately 15 % of the landmass in the Northern Hemisphere and is becoming more susceptible to rapid thawing as the climate continues to warm (Obu et al. 2019). When ice-rich permafrost thaws it can alter the surface characteristics of a landscape which is commonly referred to as thermokarst. Retrogressive Thaw Slumps (RTS) are emerging as one of the most dynamic types of thermokarst, varying strongly in shape and thawing behavior. The prevalence and distribution of rapid thaw on a pan-Arctic scale are not well understood and so is its potential contribution in the Arctic carbon-climate feedback (Kokelj et al. 2009). High-resolution Digital Elevation Models (DEMs) are a valuable tool for monitoring surface characteristics of thermokarst features and track changes over time, which in turn improves our understanding of ... Text Arctic Ice Mackenzie river permafrost Thermokarst DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
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Permafrost Retrogressive Thaw Slumps DEM infoeu-repo/classification/ddc/550 Earth sciences |
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Permafrost Retrogressive Thaw Slumps DEM infoeu-repo/classification/ddc/550 Earth sciences Maier, Kathrin Bernhard, Philipp Hajnsek, Irena Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
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Permafrost Retrogressive Thaw Slumps DEM infoeu-repo/classification/ddc/550 Earth sciences |
description |
Permafrost is a common characteristic of Arctic landscapes, where it refers to ground that remains at or below 0 °C for a duration of at least two consecutive years. Permafrost underlies approximately 15 % of the landmass in the Northern Hemisphere and is becoming more susceptible to rapid thawing as the climate continues to warm (Obu et al. 2019). When ice-rich permafrost thaws it can alter the surface characteristics of a landscape which is commonly referred to as thermokarst. Retrogressive Thaw Slumps (RTS) are emerging as one of the most dynamic types of thermokarst, varying strongly in shape and thawing behavior. The prevalence and distribution of rapid thaw on a pan-Arctic scale are not well understood and so is its potential contribution in the Arctic carbon-climate feedback (Kokelj et al. 2009). High-resolution Digital Elevation Models (DEMs) are a valuable tool for monitoring surface characteristics of thermokarst features and track changes over time, which in turn improves our understanding of ... |
format |
Text |
author |
Maier, Kathrin Bernhard, Philipp Hajnsek, Irena |
author_facet |
Maier, Kathrin Bernhard, Philipp Hajnsek, Irena |
author_sort |
Maier, Kathrin |
title |
Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
title_short |
Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
title_full |
Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
title_fullStr |
Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
title_full_unstemmed |
Assessing TanDEM-X-Derived Digital Elevation Models for Monitoring Rapid Permafrost Thaw: A Case Study in the Mackenzie River Delta ... |
title_sort |
assessing tandem-x-derived digital elevation models for monitoring rapid permafrost thaw: a case study in the mackenzie river delta ... |
publisher |
ETH Zurich |
publishDate |
2023 |
url |
https://dx.doi.org/10.3929/ethz-b-000655439 http://hdl.handle.net/20.500.11850/655439 |
genre |
Arctic Ice Mackenzie river permafrost Thermokarst |
genre_facet |
Arctic Ice Mackenzie river permafrost Thermokarst |
op_doi |
https://doi.org/10.3929/ethz-b-000655439 |
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1797576850062442496 |