Lower soil moisture and deep soil temperatures in thermokarst features increase old soil carbon loss after 10 years of experimental permafrost warming-Reference-Cited by-同舟云学术

Lower soil moisture and deep soil temperatures in thermokarst features increase old soil carbon loss after 10 years of experimental permafrost warming

Published:2020-12-24 Issue:6 Volume:27 Page:1293-1308
ISSN:1354-1013
Container-title:Global Change Biology
language:en
Short-container-title:Glob. Change Biol.

Author:

Pegoraro Elaine F.¹²^ORCID,Mauritz Marguerite E.³^ORCID,Ogle Kiona¹⁴^ORCID,Ebert Christopher H.¹^ORCID,Schuur Edward A. G.¹²^ORCID

Affiliation:

1. Center for Ecosystem Science and Society Northern Arizona University Flagstaff AZ USA

2. Biological Sciences Northern Arizona University Flagstaff AZ USA

3. Ecology and Evolutionary Biology The University of Texas at El Paso El Paso TX USA

4. School of Informatics, Computing, and Cyber Systems Northern Arizona University Flagstaff AZ USA

Funder

U.S. Department of Energy

National Science Foundation

Sigma Xi

Publisher

Wiley

Subject

General Environmental Science,Ecology,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15481

Reference91 articles.

1. Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire: an expert assessment

2. Thermal Properties of Soils as affected by Density and Water Content

3. Soil Thermal Conductivity Effects of Density, Moisture, Salt Concentration, and Organic Matter

4. Fitting Linear Mixed-Effects Models Usinglme4

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