Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Stiig Wilkenskjeld"'
Autor:
Roger C. Creel, Frederieke Miesner, Stiig Wilkenskjeld, Jacqueline Austermann, Pier Paul Overduin
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-14 (2024)
Abstract Sea-level rise submerges terrestrial permafrost in the Arctic, turning it into subsea permafrost. Subsea permafrost underlies ~ 1.8 million km2 of Arctic continental shelf, with thicknesses in places exceeding 700 m. Sea-level variations ove
Externí odkaz:
https://doaj.org/article/5dc2dd4d82914131aa775561a48e3c6d
Autor:
Thorsten Mauritsen, Jürgen Bader, Tobias Becker, Jörg Behrens, Matthias Bittner, Renate Brokopf, Victor Brovkin, Martin Claussen, Traute Crueger, Monika Esch, Irina Fast, Stephanie Fiedler, Dagmar Fläschner, Veronika Gayler, Marco Giorgetta, Daniel S. Goll, Helmuth Haak, Stefan Hagemann, Christopher Hedemann, Cathy Hohenegger, Tatiana Ilyina, Thomas Jahns, Diego Jimenéz‐de‐la‐Cuesta, Johann Jungclaus, Thomas Kleinen, Silvia Kloster, Daniela Kracher, Stefan Kinne, Deike Kleberg, Gitta Lasslop, Luis Kornblueh, Jochem Marotzke, Daniela Matei, Katharina Meraner, Uwe Mikolajewicz, Kameswarrao Modali, Benjamin Möbis, Wolfgang A. Müller, Julia E. M. S. Nabel, Christine C. W. Nam, Dirk Notz, Sarah‐Sylvia Nyawira, Hanna Paulsen, Karsten Peters, Robert Pincus, Holger Pohlmann, Julia Pongratz, Max Popp, Thomas Jürgen Raddatz, Sebastian Rast, Rene Redler, Christian H. Reick, Tim Rohrschneider, Vera Schemann, Hauke Schmidt, Reiner Schnur, Uwe Schulzweida, Katharina D. Six, Lukas Stein, Irene Stemmler, Bjorn Stevens, Jin‐Song vonStorch, Fangxing Tian, Aiko Voigt, Philipp Vrese, Karl‐Hermann Wieners, Stiig Wilkenskjeld, Alexander Winkler, Erich Roeckner
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 4, Pp 998-1038 (2019)
Abstract A new release of the Max Planck Institute for Meteorology Earth System Model version 1.2 (MPI‐ESM1.2) is presented. The development focused on correcting errors in and improving the physical processes representation, as well as improving t
Externí odkaz:
https://doaj.org/article/0933f7e3611440809988d07078c822a0
Autor:
Philipp de Vrese, Goran Georgievski, Jesus Fidel Gonzalez Rouco, Dirk Notz, Tobias Stacke, Norman Julius Steinert, Stiig Wilkenskjeld, Victor Brovkin
Publikováno v:
The Cryosphere
The current generation of Earth system models exhibits large inter-model differences in the simulated climate of the Arctic and subarctic zone, with differences in model structure and parametrizations being one of the main sources of uncertainty. One
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2d4fe582acda926771beb4662351035c
https://hdl.handle.net/21.11116/0000-000D-09A8-C21.11116/0000-000D-43FC-C
https://hdl.handle.net/21.11116/0000-000D-09A8-C21.11116/0000-000D-43FC-C
Sea-level rise submerges terrestrial permafrost in the Arctic, turning it into subsea permafrost. Subsea permafrost underlies ∼1.8 million km^2 of Arctic continental shelf, with thicknesses in places exceeding 700 m. Sea-level variations over glaci
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f64504a992cd8536c9eca65ab9c12bb
https://doi.org/10.31223/x55q2z
https://doi.org/10.31223/x55q2z
Publikováno v:
The Cryosphere
Most earth system models (ESMs) neglect climate feedbacks arising from carbon release from thawing permafrost, especially from thawing of subsea permafrost (SSPF). To assess the fate of SSPF in the next 1000 years, we implemented SSPF into JSBACH, th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::110b8b7f280cc8b709d9279fb07fce19
https://doi.org/10.5194/tc-16-1057-2022
https://doi.org/10.5194/tc-16-1057-2022
Autor:
Philipp de Vrese, Goran Georgievski, Jesus Fidel Gonzalez Rouco, Dirk Notz, Tobias Stacke, Norman Julius Steinert, Stiig Wilkenskjeld, Victor Brovkin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e7dd30feda84438454b22cbe53903162
https://doi.org/10.5194/tc-2022-150-supplement
https://doi.org/10.5194/tc-2022-150-supplement
Most Earth System Models (ESMs) neglect climate feedbacks arising from carbon release from thawing permafrost, especially from thawing of sub-sea permafrost (SSPF). To assess the fate of SSPF in the next 1000 years, we implemented SSPF into JSBACH, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3f722272a9c0f8b5d1981e0f3a87ca99
https://tc.copernicus.org/preprints/tc-2021-231/
https://tc.copernicus.org/preprints/tc-2021-231/