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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| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
JOHN WILEY & SONS LTD
2014
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| Subjects: | |
| 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 |
| Summary: | 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. |
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