Permafrost thermal regime from two 30‐m deep boreholes in southern victoria land, antarctica
Two 30‐m deep permafrost temperature‐monitoring boreholes were installed in bedrock, one at Marble Point and one in the Wright Valley, in the Ross Sea region of Antarctica. A soil climate‐monitoring station in till is located near each borehole. The ground surface temperature (GST) was highly correl...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.715 |
Summary: | Two 30‐m deep permafrost temperature‐monitoring boreholes were installed in bedrock, one at Marble Point and one in the Wright Valley, in the Ross Sea region of Antarctica. A soil climate‐monitoring station in till is located near each borehole. The ground surface temperature (GST) was highly correlated with the air temperature at both sites in 2008. Thermal offsets were small ( |
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