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ARCSS/TK Project

Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The "TK" in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...

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Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The TK in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...
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ARCSS/TK Project | arcss-tk.blogspot.com Reviews

https://arcss-tk.blogspot.com

Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The "TK" in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...

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1

ARCSS/TK Project: Who am I and what is ARCSS/TK?

http://www.arcss-tk.blogspot.com/2009/06/who-am-i-and-what-is-arcsstk.html

Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The "TK" in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...

2

ARCSS/TK Project: June 2009

http://www.arcss-tk.blogspot.com/2009_06_01_archive.html

Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The "TK" in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...

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ARCSS/TK Field Sites Blog. Running log of activities at the field sites of the ARCSS/TK research project. Friday, July 3, 2009. Lewkowicz, Gooseff, and Godsey deployed 6 ground temperature monitoring stations and a met station from 25 Jun to 26 Jun. All sensors except soil moisture sensors were functional as of 01 Jul. All measurements are being recorded hourly. We are also monitoring soil moisture at 0, 20, and 40 cm deep at 3 stations, all of which are outside of the gulley. Solar radiation (short wave).

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ARCSS/TK Project

Information and observations about an US/NSF-sponsored collaborative research project to better understand how climate warming might influence the arctic landscape. Friday, June 26, 2009. Who am I and what is ARCSS/TK? But this blog is not primarily intended to be about me. The "TK" in our name. Permanently frozen soil. A thin layer of soil on the top will thaw each year - the active layer. As you might imagine, the frozen soil is hard. But if the permafrost warms and thaws, the once-frozen soil lose...

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