doi:[removed]1088937x[removed]

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Date: 2014-08-30 18:56:13 Earth Permafrost Active layer Soil Urban heat island Thaw depth Barrow Alaska Cryoturbation Gelisols Physical geography Pedology Geography		doi:[removed]1088937x[removed] Add to Reading List Source URL: www.cas.umt.edu Download Document from Source Website File Size: 4,00 MB Share Document on Facebook

	The Importance of “Deep” Organic Carbon in Permafrost-Affected Soils of Arctic Alaska J. G. Bockheim* Dep. of Soil Science Univ. of Wisconsin DocID: 1q7TA - View Document
	Microsoft Word130222 DocID: 1g6CN - View Document
	This discussion paper is/has been under review for the journal The Cryosphere (TC). Please refer to the corresponding final paper in TC if available. Discussion Paper The Cryosphere Discuss., 9, 3137–3163, 2015 DocID: 1fSam - View Document
	Geosci. Model Dev., 8, 1493–1508, 2015 www.geosci-model-dev.netdoi:gmd © Author(sCC Attribution 3.0 License. An improved representation of physical permafrost dynamics in the DocID: 19ARj - View Document
	Biogeosciences, 12, 3119–3130, 2015 www.biogeosciences.netdoi:bg © Author(sCC Attribution 3.0 License. Environmental correlates of peatland carbon fluxes in a thawing DocID: 19xAe - View Document