Spatial and temporal changes in soil climate and active layer depth in the Ross Sea Region, Antarctica, 1999-2018
The depth of seasonal thaw (the active layer depth) integrates a range of soil and atmospheric climate variables and has potential to provide a clear signal of a changing climate. Nine soil climate monitoring stations (SCS) were established between 1999 and 2012 and are currently operating in the Ro...
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Other Authors: | , , |
Format: | Thesis |
Language: | English |
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The University of Waikato
2020
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Online Access: | https://hdl.handle.net/10289/13519 |