Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits
Wedge-ice volume (WIV) is a key factor in assessing the response of ice-rich permafrost landscapes to thaw and in quantifying deep permafrost soil carbon inventories. Here, we present a method for calculating WIV in late Pleistocene Yedoma deposits and Holocene thermokarst basin deposits at four stu...
Published in: | Permafrost and Periglacial Processes |
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JOHN WILEY & SONS LTD
2014
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Online Access: | https://epic.awi.de/id/eprint/35710/ https://epic.awi.de/id/eprint/35710/1/Abstract_Quantifying_Wedge_Ice.pdf http://onlinelibrary.wiley.com/doi/10.1002/ppp.1810/abstract https://hdl.handle.net/10013/epic.43642 https://hdl.handle.net/10013/epic.43642.d001 |
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ftawi:oai:epic.awi.de:35710 2023-05-15T16:36:49+02:00 Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits Ulrich, Mathias Grosse, Guido Strauss, Jens Schirrmeister, Lutz 2014-06-04 application/pdf https://epic.awi.de/id/eprint/35710/ https://epic.awi.de/id/eprint/35710/1/Abstract_Quantifying_Wedge_Ice.pdf http://onlinelibrary.wiley.com/doi/10.1002/ppp.1810/abstract https://hdl.handle.net/10013/epic.43642 https://hdl.handle.net/10013/epic.43642.d001 unknown JOHN WILEY & SONS LTD https://epic.awi.de/id/eprint/35710/1/Abstract_Quantifying_Wedge_Ice.pdf https://hdl.handle.net/10013/epic.43642.d001 Ulrich, M. , Grosse, G. orcid:0000-0001-5895-2141 , Strauss, J. orcid:0000-0003-4678-4982 and Schirrmeister, L. orcid:0000-0001-9455-0596 (2014) Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits , Permafrost and Periglacial Processes . doi:10.1002/ppp.1810 <https://doi.org/10.1002/ppp.1810> , hdl:10013/epic.43642 info:eu-repo/semantics/openAccess EPIC3Permafrost and Periglacial Processes, JOHN WILEY & SONS LTD, ISSN: 1045-6740 Article isiRev info:eu-repo/semantics/article 2014 ftawi https://doi.org/10.1002/ppp.1810 2021-12-24T15:39:35Z Wedge-ice volume (WIV) is a key factor in assessing the response of ice-rich permafrost landscapes to thaw and in quantifying deep permafrost soil carbon inventories. Here, we present a method for calculating WIV in late Pleistocene Yedoma deposits and Holocene thermokarst basin deposits at four study areas in Siberia and Alaska. Ice-wedge polygons and thermokarst mound (baydzherakh) patterns were mapped on different landscape units using very high-resolution (0.5 m/pixel) satellite imagery (WorldView-1 and GeoEye-1). In a geographic information system (GIS) environment, Thiessen polygons were automatically created to reconstruct relict ice-wedge polygonal networks, and field and published data on ice-wedge dimensions were used to generate three-dimensional subsurface models that distinguish between epi- and syngenetic ice-wedge geometry. The results reveal significant variations in WIV between the study sites and within certain terrain units. Calculated maximum WIV ranges from 31.4 to 63.2 vol% for Yedoma deposits and from 6.6 to 13.2 vol% for thermokarst basin deposits. Article in Journal/Newspaper Ice permafrost Permafrost and Periglacial Processes Thermokarst wedge* Alaska Siberia Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Permafrost and Periglacial Processes 25 3 151 161 |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
language |
unknown |
description |
Wedge-ice volume (WIV) is a key factor in assessing the response of ice-rich permafrost landscapes to thaw and in quantifying deep permafrost soil carbon inventories. Here, we present a method for calculating WIV in late Pleistocene Yedoma deposits and Holocene thermokarst basin deposits at four study areas in Siberia and Alaska. Ice-wedge polygons and thermokarst mound (baydzherakh) patterns were mapped on different landscape units using very high-resolution (0.5 m/pixel) satellite imagery (WorldView-1 and GeoEye-1). In a geographic information system (GIS) environment, Thiessen polygons were automatically created to reconstruct relict ice-wedge polygonal networks, and field and published data on ice-wedge dimensions were used to generate three-dimensional subsurface models that distinguish between epi- and syngenetic ice-wedge geometry. The results reveal significant variations in WIV between the study sites and within certain terrain units. Calculated maximum WIV ranges from 31.4 to 63.2 vol% for Yedoma deposits and from 6.6 to 13.2 vol% for thermokarst basin deposits. |
format |
Article in Journal/Newspaper |
author |
Ulrich, Mathias Grosse, Guido Strauss, Jens Schirrmeister, Lutz |
spellingShingle |
Ulrich, Mathias Grosse, Guido Strauss, Jens Schirrmeister, Lutz Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
author_facet |
Ulrich, Mathias Grosse, Guido Strauss, Jens Schirrmeister, Lutz |
author_sort |
Ulrich, Mathias |
title |
Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
title_short |
Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
title_full |
Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
title_fullStr |
Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
title_full_unstemmed |
Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
title_sort |
quantifying wedge-ice volumes in yedoma and thermokarst basin deposits |
publisher |
JOHN WILEY & SONS LTD |
publishDate |
2014 |
url |
https://epic.awi.de/id/eprint/35710/ https://epic.awi.de/id/eprint/35710/1/Abstract_Quantifying_Wedge_Ice.pdf http://onlinelibrary.wiley.com/doi/10.1002/ppp.1810/abstract https://hdl.handle.net/10013/epic.43642 https://hdl.handle.net/10013/epic.43642.d001 |
genre |
Ice permafrost Permafrost and Periglacial Processes Thermokarst wedge* Alaska Siberia |
genre_facet |
Ice permafrost Permafrost and Periglacial Processes Thermokarst wedge* Alaska Siberia |
op_source |
EPIC3Permafrost and Periglacial Processes, JOHN WILEY & SONS LTD, ISSN: 1045-6740 |
op_relation |
https://epic.awi.de/id/eprint/35710/1/Abstract_Quantifying_Wedge_Ice.pdf https://hdl.handle.net/10013/epic.43642.d001 Ulrich, M. , Grosse, G. orcid:0000-0001-5895-2141 , Strauss, J. orcid:0000-0003-4678-4982 and Schirrmeister, L. orcid:0000-0001-9455-0596 (2014) Quantifying wedge-ice volumes in yedoma and thermokarst basin deposits , Permafrost and Periglacial Processes . doi:10.1002/ppp.1810 <https://doi.org/10.1002/ppp.1810> , hdl:10013/epic.43642 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1002/ppp.1810 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
25 |
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3 |
container_start_page |
151 |
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161 |
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