Zobrazeno 1 - 10
of 107
pro vyhledávání: '"T. Hattermann"'
Autor:
N. C. Swart, T. Martin, R. Beadling, J.-J. Chen, C. Danek, M. H. England, R. Farneti, S. M. Griffies, T. Hattermann, J. Hauck, F. A. Haumann, A. Jüling, Q. Li, J. Marshall, M. Muilwijk, A. G. Pauling, A. Purich, I. J. Smith, M. Thomas
Publikováno v:
Geoscientific Model Development, Vol 16, Pp 7289-7309 (2023)
As the climate warms, the grounded ice sheet and floating ice shelves surrounding Antarctica are melting and releasing additional freshwater into the Southern Ocean. Nonetheless, almost all existing coupled climate models have fixed ice sheets and la
Externí odkaz:
https://doaj.org/article/1fc3a6a5e47f4fb4b2e95ffd97f42b41
Publikováno v:
The Cryosphere, Vol 17, Pp 5255-5281 (2023)
One of the last remaining floating tongues of the Greenland ice sheet (GrIS), the Petermann Glacier ice shelf (PGIS), is seasonally shielded from warm Atlantic water (AW) by the formation of sea ice arches in the Nares Strait. However, continued decl
Externí odkaz:
https://doaj.org/article/bd3c54bed3f7401fa1a5807458244441
Autor:
H. Seroussi, V. Verjans, S. Nowicki, A. J. Payne, H. Goelzer, W. H. Lipscomb, A. Abe-Ouchi, C. Agosta, T. Albrecht, X. Asay-Davis, A. Barthel, R. Calov, R. Cullather, C. Dumas, B. K. Galton-Fenzi, R. Gladstone, N. R. Golledge, J. M. Gregory, R. Greve, T. Hattermann, M. J. Hoffman, A. Humbert, P. Huybrechts, N. C. Jourdain, T. Kleiner, E. Larour, G. R. Leguy, D. P. Lowry, C. M. Little, M. Morlighem, F. Pattyn, T. Pelle, S. F. Price, A. Quiquet, R. Reese, N.-J. Schlegel, A. Shepherd, E. Simon, R. S. Smith, F. Straneo, S. Sun, L. D. Trusel, J. Van Breedam, P. Van Katwyk, R. S. W. van de Wal, R. Winkelmann, C. Zhao, T. Zhang, T. Zwinger
Publikováno v:
The Cryosphere, Vol 17, Pp 5197-5217 (2023)
The Antarctic Ice Sheet represents the largest source of uncertainty in future sea level rise projections, with a contribution to sea level by 2100 ranging from −5 to 43 cm of sea level equivalent under high carbon emission scenarios estimated by t
Externí odkaz:
https://doaj.org/article/602d0106f5dc44e2a4a46926008676ae
Autor:
J. Gutt, S. Arndt, D. K. A. Barnes, H. Bornemann, T. Brey, O. Eisen, H. Flores, H. Griffiths, C. Haas, S. Hain, T. Hattermann, C. Held, M. Hoppema, E. Isla, M. Janout, C. Le Bohec, H. Link, F. C. Mark, S. Moreau, S. Trimborn, I. van Opzeeland, H.-O. Pörtner, F. Schaafsma, K. Teschke, S. Tippenhauer, A. Van de Putte, M. Wege, D. Zitterbart, D. Piepenburg
Publikováno v:
Biogeosciences, Vol 19, Pp 5313-5342 (2022)
Systematic long-term studies on ecosystem dynamics are largely lacking from the East Antarctic Southern Ocean, although it is well recognized that they are indispensable to identify the ecological impacts and risks of environmental change. Here, we p
Externí odkaz:
https://doaj.org/article/abd330f9342c4580bf6cf8756fa5bff1
Publikováno v:
Geoscientific Model Development, Vol 15, Pp 5421-5439 (2022)
Changes in ocean-driven basal melting have a key influence on the stability of ice shelves, the mass loss from the ice sheet, ocean circulation, and global sea level rise. Coupled ice sheet–ocean models play a critical role in understanding future
Externí odkaz:
https://doaj.org/article/4a1c183d57844f36808317ad6144e0fd
Autor:
C. Hofstede, S. Beyer, H. Corr, O. Eisen, T. Hattermann, V. Helm, N. Neckel, E. C. Smith, D. Steinhage, O. Zeising, A. Humbert
Publikováno v:
The Cryosphere, Vol 15, Pp 1517-1535 (2021)
Curvilinear channels on the surface of an ice shelf indicate the presence of large channels at the base. Modelling studies have shown that where these surface expressions intersect the grounding line, they coincide with the likely outflow of subglaci
Externí odkaz:
https://doaj.org/article/3416ac1b9cb44c00975511c71e6acaf0
Autor:
R. Gladstone, B. Galton-Fenzi, D. Gwyther, Q. Zhou, T. Hattermann, C. Zhao, L. Jong, Y. Xia, X. Guo, K. Petrakopoulos, T. Zwinger, D. Shapero, J. Moore
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 889-905 (2021)
A number of important questions concern processes at the margins of ice sheets where multiple components of the Earth system, most crucially ice sheets and oceans, interact. Such processes include thermodynamic interaction at the ice–ocean interfac
Externí odkaz:
https://doaj.org/article/bed6bfeceb1c4abe8f973c32a792e1a3
Publikováno v:
Ocean Science, Vol 16, Pp 1225-1246 (2020)
Fram Strait, the deepest gateway to the Arctic Ocean, is strongly influenced by eddy dynamics. Here we analyse the output from two eddy-resolving models (ROMS – Regional Ocean Modeling System; FESOM – Finite-Element Sea-ice Ocean Model) with arou
Externí odkaz:
https://doaj.org/article/1cd42702a5bc46cb9abd42d5f211e598
ISMIP6 Antarctica: a multi-model ensemble of the Antarctic ice sheet evolution over the 21st century
Autor:
H. Seroussi, S. Nowicki, A. J. Payne, H. Goelzer, W. H. Lipscomb, A. Abe-Ouchi, C. Agosta, T. Albrecht, X. Asay-Davis, A. Barthel, R. Calov, R. Cullather, C. Dumas, B. K. Galton-Fenzi, R. Gladstone, N. R. Golledge, J. M. Gregory, R. Greve, T. Hattermann, M. J. Hoffman, A. Humbert, P. Huybrechts, N. C. Jourdain, T. Kleiner, E. Larour, G. R. Leguy, D. P. Lowry, C. M. Little, M. Morlighem, F. Pattyn, T. Pelle, S. F. Price, A. Quiquet, R. Reese, N.-J. Schlegel, A. Shepherd, E. Simon, R. S. Smith, F. Straneo, S. Sun, L. D. Trusel, J. Van Breedam, R. S. W. van de Wal, R. Winkelmann, C. Zhao, T. Zhang, T. Zwinger
Publikováno v:
The Cryosphere, Vol 14, Pp 3033-3070 (2020)
Ice flow models of the Antarctic ice sheet are commonly used to simulate its future evolution in response to different climate scenarios and assess the mass loss that would contribute to future sea level rise. However, there is currently no consensus
Externí odkaz:
https://doaj.org/article/2e30e29db70c4a43b7f755af333da47b
Autor:
N. C. Jourdain, X. Asay-Davis, T. Hattermann, F. Straneo, H. Seroussi, C. M. Little, S. Nowicki
Publikováno v:
The Cryosphere, Vol 14, Pp 3111-3134 (2020)
Climate model projections have previously been used to compute ice shelf basal melt rates in ice sheet models, but the strategies employed – e.g., ocean input, parameterization, calibration technique, and corrections – have varied widely and are
Externí odkaz:
https://doaj.org/article/dc8874c79aec4d5cae945531bcd2d295