USAP-DC

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Active Layer Temperatures from Crescent Stream banks, Taylor Valley Antarctica Data DOI: https://doi.org/10.15784/601075 Cite as Gooseff, M. N. (2017) "Active Layer Temperatures from Crescent Stream banks, Taylor Valley Antarctica" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/10.15784/601075. AMD - DIF Record(s) USAP-1246203 Abstract As a part of the project titled "Collaborative Research: The McMurdo Dry Valleys: A landscape on the threshold of change", we measured ground temperatures from 0-20cm at three stream bank positions (base, mid-slope, and top) at 4 locations along Crescent Stream in Taylor Valley - 2 on the east bank, 2 on the west bank. The goal was to evaluate differences in thermal conduction and temperature dynamics of the active layers of these locations, in particular, in a stream that has undergone extensive bank erosion since 2012 due to permafrost degradation. One of the datalogging stations had significant technical problems and has very little data compared to the almost 2 years of temperature date from the other 3 stations (2015-2017). Creator(s): Gooseff, Michael N. Date Created: 2017-12-18 Repository: USAP-DC (current) License: Creative Commons Attribution-NonCommercial v4.0 Generic [CC BY-NC 4.0] Spatial Extent(s) West: 163.1778, East: 163.179, South: -77.7234, North: -77.6233 Temporal Extent(s) Start: 2015-01-01 - End: 2017-01-31 Award(s) NSF 1246203 Version: 1 Related Project(s) Collaborative Research: THE MCMURDO DRY VALLEYS: A landscape on the Threshold of Change Keywords Antarctica Dry Valleys Glaciology Paleoclimate Permafrost Soil Temperature Taylor Valley