Observations and modelling of ground temperature evolution in the discontinuous permafrost zone in Nadym, north‐west Siberia

Author:

Kukkonen Ilmo T.1ORCID,Suhonen Elli1ORCID,Ezhova Ekaterina1ORCID,Lappalainen Hanna12,Gennadinik Victor3ORCID,Ponomareva Olga45,Gravis Andrey4ORCID,Miles Victoria6ORCID,Kulmala Markku13ORCID,Melnikov Vladimir378ORCID,Drozdov Dmitry345

Affiliation:

1. University of Helsinki Helsinki Finland

2. Finnish Meteorological Institute Helsinki Finland

3. Tyumen State University Tyumen Russia

4. Earth Cryosphere Institute SB RAS Moscow Russia

5. MGRI Moscow Russia

6. Nansen Environmental and Remote Sensing Center Bergen Norway

7. Tyumen Industrial University Tyumen Russia

8. Earth Cryosphere Institute SB RAS Tyumen Russia

Funder

Russian Academy of Sciences

Publisher

Wiley

Subject

Earth-Surface Processes

Reference53 articles.

1. Numerical simulation of permafrost evolution as a part of sedimentary basin modeling: permafrost in the Pliocene–Holocene climate history of the Urengoy field in the West Siberian basin

2. Changes in the extent of permafrost during the late quaternary period in the territory of the former Soviet Union

3. MelnikovVP DrozdovDS PendinVV.Arctic Permafrost: Dynamics Risks Problems and Solutions. Moscow XXII Int. Science‐Practical Conf. "New Ideas In Earth Science" 8–10.04.2015. Moscow;2015:123–138.

4. MelnikovVV PendinDS DrozdovDS.Development of extreme events over technogenic structures in permafrost zone: natural risks//international conference on silk‐roads disaster risk reduction and sustainable development. May 11–12 2019 Beijing International Convention Center China (in press);2019.

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