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 |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.1810 |
id |
ftrepec:oai:RePEc:wly:perpro:v:25:y:2014:i:3:p:151-161 |
---|---|
record_format |
openpolar |
spelling |
ftrepec:oai:RePEc:wly:perpro:v:25:y:2014:i:3:p:151-161 2023-05-15T16:36:49+02:00 Quantifying Wedge‐Ice Volumes in Yedoma and Thermokarst Basin Deposits Mathias Ulrich Guido Grosse Jens Strauss Lutz Schirrmeister https://doi.org/10.1002/ppp.1810 unknown https://doi.org/10.1002/ppp.1810 article ftrepec https://doi.org/10.1002/ppp.1810 2020-12-04T13:31:25Z 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. Copyright © 2014 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice permafrost Thermokarst wedge* Alaska Siberia RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 25 3 151 161 |
institution |
Open Polar |
collection |
RePEc (Research Papers in Economics) |
op_collection_id |
ftrepec |
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. Copyright © 2014 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Mathias Ulrich Guido Grosse Jens Strauss Lutz Schirrmeister |
spellingShingle |
Mathias Ulrich Guido Grosse Jens Strauss Lutz Schirrmeister Quantifying Wedge‐Ice Volumes in Yedoma and Thermokarst Basin Deposits |
author_facet |
Mathias Ulrich Guido Grosse Jens Strauss Lutz Schirrmeister |
author_sort |
Mathias Ulrich |
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 |
url |
https://doi.org/10.1002/ppp.1810 |
genre |
Ice permafrost Thermokarst wedge* Alaska Siberia |
genre_facet |
Ice permafrost Thermokarst wedge* Alaska Siberia |
op_relation |
https://doi.org/10.1002/ppp.1810 |
op_doi |
https://doi.org/10.1002/ppp.1810 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
25 |
container_issue |
3 |
container_start_page |
151 |
op_container_end_page |
161 |
_version_ |
1766027137848967168 |