Zobrazeno 1 - 10
of 14
pro vyhledávání: '"O. Gurses"'
Autor:
D. Sidorenko, H.F. Goessling, N.V. Koldunov, P. Scholz, S. Danilov, D. Barbi, W. Cabos, O. Gurses, S. Harig, C. Hinrichs, S. Juricke, G. Lohmann, M. Losch, L. Mu, T. Rackow, N. Rakowsky, D. Sein, T. Semmler, X. Shi, C. Stepanek, J. Streffing, Q. Wang, C. Wekerle, H. Yang, T. Jung
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 11, Iss 11, Pp 3794-3815 (2019)
Abstract A new global climate model setup using FESOM2.0 for the sea ice‐ocean component and ECHAM6.3 for the atmosphere and land surface has been developed. Replacing FESOM1.4 by FESOM2.0 promises a higher efficiency of the new climate setup compa
Externí odkaz:
https://doaj.org/article/788031fb96614560af7484ebb868377d
Autor:
P. Scholz, D. Sidorenko, O. Gurses, S. Danilov, N. Koldunov, Q. Wang, D. Sein, M. Smolentseva, N. Rakowsky, T. Jung
Publikováno v:
Geoscientific Model Development, Vol 12, Pp 4875-4899 (2019)
The evaluation and model element description of the second version of the unstructured-mesh Finite-volumE Sea ice-Ocean Model (FESOM2.0) are presented. The new version of the model takes advantage of the finite-volume approach, whereas its predecesso
Externí odkaz:
https://doaj.org/article/5964c5f397654096b7404d3d38093c21
Publikováno v:
Geoscientific Model Development, Vol 17, Pp 1709-1727 (2024)
In this paper we describe the implementation of the carbon isotopes 13C and 14C (radiocarbon) into the marine biogeochemistry model REcoM3. The implementation is tested in long-term equilibrium simulations where REcoM3 is coupled with the ocean gener
Externí odkaz:
https://doaj.org/article/b05ea63a6ba44c56b00ff7359f4290a7
Publikováno v:
Ocean Science, Vol 19, Pp 1529-1544 (2023)
Recent studies have found evidence for a potential future tipping point, when the density of Antarctic continental shelf waters, specifically in the southern Weddell Sea, will allow for the onshore flow of warm waters of open ocean origin. A cold-to-
Externí odkaz:
https://doaj.org/article/3ebe0fcb437e45909f305a408e44ba5b
Autor:
Ö. Gürses, L. Oziel, O. Karakuş, D. Sidorenko, C. Völker, Y. Ye, M. Zeising, M. Butzin, J. Hauck
Publikováno v:
Geoscientific Model Development, Vol 16, Pp 4883-4936 (2023)
The cycling of carbon in the oceans is affected by feedbacks driven by changes in climate and atmospheric CO2. Understanding these feedbacks is therefore an important prerequisite for projecting future climate. Marine biogeochemistry models are a use
Externí odkaz:
https://doaj.org/article/b4a1e1fd8a634c39a4e2a852490f5b44
Autor:
P. Friedlingstein, M. W. Jones, M. O'Sullivan, R. M. Andrew, D. C. E. Bakker, J. Hauck, C. Le Quéré, G. P. Peters, W. Peters, J. Pongratz, S. Sitch, J. G. Canadell, P. Ciais, R. B. Jackson, S. R. Alin, P. Anthoni, N. R. Bates, M. Becker, N. Bellouin, L. Bopp, T. T. T. Chau, F. Chevallier, L. P. Chini, M. Cronin, K. I. Currie, B. Decharme, L. M. Djeutchouang, X. Dou, W. Evans, R. A. Feely, L. Feng, T. Gasser, D. Gilfillan, T. Gkritzalis, G. Grassi, L. Gregor, N. Gruber, Ö. Gürses, I. Harris, R. A. Houghton, G. C. Hurtt, Y. Iida, T. Ilyina, I. T. Luijkx, A. Jain, S. D. Jones, E. Kato, D. Kennedy, K. Klein Goldewijk, J. Knauer, J. I. Korsbakken, A. Körtzinger, P. Landschützer, S. K. Lauvset, N. Lefèvre, S. Lienert, J. Liu, G. Marland, P. C. McGuire, J. R. Melton, D. R. Munro, J. E. M. S. Nabel, S.-I. Nakaoka, Y. Niwa, T. Ono, D. Pierrot, B. Poulter, G. Rehder, L. Resplandy, E. Robertson, C. Rödenbeck, T. M. Rosan, J. Schwinger, C. Schwingshackl, R. Séférian, A. J. Sutton, C. Sweeney, T. Tanhua, P. P. Tans, H. Tian, B. Tilbrook, F. Tubiello, G. R. van der Werf, N. Vuichard, C. Wada, R. Wanninkhof, A. J. Watson, D. Willis, A. J. Wiltshire, W. Yuan, C. Yue, X. Yue, S. Zaehle, J. Zeng
Publikováno v:
Earth System Science Data, Vol 14, Pp 1917-2005 (2022)
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the developmen
Externí odkaz:
https://doaj.org/article/c709ef6e046f42c5b3697a99222ac117
Publikováno v:
Earth System Dynamics, Vol 11, Pp 1153-1194 (2020)
Various observational estimates indicate growing mass loss at Antarctica's margins as well as heavier precipitation across the continent. Simulated future projections reveal that heavier precipitation, falling on Antarctica, may counteract amplified
Externí odkaz:
https://doaj.org/article/0ce30c7b45fe49bbb744b33951ebe859
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Publikováno v:
The Cryosphere, Vol 13, Pp 2317-2324 (2019)
Disintegration of ice shelves in the Amundsen Sea, in front of the West Antarctic Ice Sheet, has the potential to cause sea level rise by inducing an acceleration of ice discharge from upstream grounded ice. Moore et al. (2018) proposed that using a
Externí odkaz:
https://doaj.org/article/df64599ba85d4af983cce03c77e48f2d
Publikováno v:
Ocean Science, Vol 14, Pp 999-1019 (2018)
A simulation of the Turkish Straits System (TSS) using a high-resolution, three-dimensional, unstructured mesh ocean circulation model with realistic atmospheric forcing for the 2008–2013 period is presented. The depth of the pycnocline between
Externí odkaz:
https://doaj.org/article/fde7e01285ab40ca94dd6bf643bc7308