Heat and Salt Flow in Subsea Permafrost Modeled with CryoGRID2-Reference-Cited by-同舟云学术

Heat and Salt Flow in Subsea Permafrost Modeled with CryoGRID2

Published:2019-04 Issue:4 Volume:124 Page:920-937
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Angelopoulos Michael¹²^ORCID,Westermann Sebastian³^ORCID,Overduin Paul¹^ORCID,Faguet Alexey⁴⁵,Olenchenko Vladimir⁴⁵^ORCID,Grosse Guido¹²^ORCID,Grigoriev Mikhail N.⁶^ORCID

Affiliation:

1. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research Potsdam Germany

2. Institute of GeosciencesUniversity of Potsdam Potsdam Germany

3. Department of GeosciencesUniversity of Oslo Oslo Norway

4. Institute of Petroleum Geology and GeophysicsRussian Academy of Sciences Novosibirsk Russia

5. Department of GeophysicsNovosibirsk State University Novosibirsk Russia

6. Melnikov Permafrost InstituteSiberian Branch, Russian Academy of Sciences Yakutsk Russia

Funder

Bundesministerium für Bildung und Forschung

Norges Forskningsråd

Russian Foundation for Basic Research

H2020 European Research Council

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JF004823

Reference62 articles.

1. Anderson D. M. Tice A. R. &McKim H. L.(1973).The unfrozen water and the apparent specific heat capacity of frozen soils. InSecond International Conference on Permafrost Yakutsk USSR. North American contribution(pp.289–295).

2. Near‐surface geophysics 2004 Society of Exploration Geophysicists Mississauga Ontario Canada A. Annan D. J. Daniels Ground‐penetrating radar 357 438

3. Composition and Flux of Holocene Sediments on the Eastern Laptev Sea Shelf, Arctic Siberia

4. Seasonal Freezing of a Subwater Ground Layer at the Laptev Sea Shelf

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