Accelerated thermokarst formation in the McMurdo Dry Valleys, Antarctica
Thermokarst is a land surface lowered and disrupted by melting ground ice. Thermokarst is a major driver of landscape change in the Arctic, but has been considered to be a minor process in Antarctica. Here, we use ground-based and airborne LiDAR coupled with timelapse imaging and meteorological data...
Published in: | Scientific Reports |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature Publishing Group
2013
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Subjects: | |
Online Access: | https://authors.library.caltech.edu/72463/ https://authors.library.caltech.edu/72463/1/srep02269.pdf https://authors.library.caltech.edu/72463/2/srep02269-s1.pdf https://authors.library.caltech.edu/72463/3/srep02269-s2.mov https://authors.library.caltech.edu/72463/4/srep02269-s3.mov https://authors.library.caltech.edu/72463/5/srep02269-s4.mov https://resolver.caltech.edu/CaltechAUTHORS:20161130-142502164 |
Summary: | Thermokarst is a land surface lowered and disrupted by melting ground ice. Thermokarst is a major driver of landscape change in the Arctic, but has been considered to be a minor process in Antarctica. Here, we use ground-based and airborne LiDAR coupled with timelapse imaging and meteorological data to show that 1) thermokarst formation has accelerated in Garwood Valley, Antarctica; 2) the rate of thermokarst erosion is presently ~ 10 times the average Holocene rate; and 3) the increased rate of thermokarst formation is driven most strongly by increasing insolation and sediment/albedo feedbacks. This suggests that sediment enhancement of insolation-driven melting may act similarly to expected increases in Antarctic air temperature (presently occurring along the Antarctic Peninsula), and may serve as a leading indicator of imminent landscape change in Antarctica that will generate thermokarst landforms similar to those in Arctic periglacial terrains. |
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