Zobrazeno 1 - 10
of 1 899
pro vyhledávání: '"T Albrecht"'
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
Publikováno v:
Earth System Dynamics, Vol 13, Pp 1077-1096 (2022)
The stability of the Greenland Ice Sheet under global warming is governed by a number of dynamic processes and interacting feedback mechanisms in the ice sheet, atmosphere and solid Earth. Here we study the long-term effects due to the interplay of t
Externí odkaz:
https://doaj.org/article/44c33f9af5114c28be5aa5ba78de0369
Autor:
Julie N. Bergmann, Rushyannah R. Killen-Cade, Lindsay A. Parish, Mark T. Albrecht, Daniel N. Wolfe
Publikováno v:
Human Vaccines & Immunotherapeutics, Vol 18, Iss 5 (2022)
On March 12, 2021, the Biomedical Advanced Research and Development Authority (BARDA) sponsored a virtual market research workshop, “Partnering on Vaccines to Counter Multi-Drug Resistant Threats,” to discuss the threat of antimicrobial resistanc
Externí odkaz:
https://doaj.org/article/77d4d95e1b204dd78d440b82dc2df73e
Publikováno v:
Geoscientific Model Development, Vol 14, Pp 3697-3714 (2021)
The past and future evolution of the Antarctic Ice Sheet is largely controlled by interactions between the ocean and floating ice shelves. To investigate these interactions, coupled ocean and ice sheet model configurations are required. Previous mode
Externí odkaz:
https://doaj.org/article/342c238232844f26bd0d3fb32d3adcca
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
Publikováno v:
The Cryosphere, Vol 14, Pp 3097-3110 (2020)
Mass loss from the Antarctic Ice Sheet constitutes the largest uncertainty in projections of future sea level rise. Ocean-driven melting underneath the floating ice shelves and subsequent acceleration of the inland ice streams are the major reasons f
Externí odkaz:
https://doaj.org/article/e2dda2262cba407181b779255cf9421d
Autor:
A. Levermann, R. Winkelmann, T. Albrecht, H. Goelzer, N. R. Golledge, R. Greve, P. Huybrechts, J. Jordan, G. Leguy, D. Martin, M. Morlighem, F. Pattyn, D. Pollard, A. Quiquet, C. Rodehacke, H. Seroussi, J. Sutter, T. Zhang, J. Van Breedam, R. Calov, R. DeConto, C. Dumas, J. Garbe, G. H. Gudmundsson, M. J. Hoffman, A. Humbert, T. Kleiner, W. H. Lipscomb, M. Meinshausen, E. Ng, S. M. J. Nowicki, M. Perego, S. F. Price, F. Saito, N.-J. Schlegel, S. Sun, R. S. W. van de Wal
Publikováno v:
Earth System Dynamics, Vol 11, Pp 35-76 (2020)
The sea level contribution of the Antarctic ice sheet constitutes a large uncertainty in future sea level projections. Here we apply a linear response theory approach to 16 state-of-the-art ice sheet models to estimate the Antarctic ice sheet contrib
Externí odkaz:
https://doaj.org/article/e6a747b9aaaf40f680e90273a5d96cc4
Publikováno v:
The Cryosphere, Vol 14, Pp 633-656 (2020)
The Parallel Ice Sheet Model (PISM) is applied to the Antarctic Ice Sheet over the last two glacial cycles (≈210 000 years) with a resolution of 16 km. An ensemble of 256 model runs is analyzed in which four relevant model parameters have been
Externí odkaz:
https://doaj.org/article/695df78a43964356a87f465b781c62a8
Publikováno v:
The Cryosphere, Vol 14, Pp 599-632 (2020)
Simulations of the glacial–interglacial history of the Antarctic Ice Sheet provide insights into dynamic threshold behavior and estimates of the ice sheet's contributions to global sea-level changes for the past, present and future. However, bounda
Externí odkaz:
https://doaj.org/article/931e902947b3432ab8f7d7dd02946ee0
Autor:
H. Seroussi, S. Nowicki, E. Simon, A. Abe-Ouchi, T. Albrecht, J. Brondex, S. Cornford, C. Dumas, F. Gillet-Chaulet, H. Goelzer, N. R. Golledge, J. M. Gregory, R. Greve, M. J. Hoffman, A. Humbert, P. Huybrechts, T. Kleiner, E. Larour, G. Leguy, W. H. Lipscomb, D. Lowry, M. Mengel, M. Morlighem, F. Pattyn, A. J. Payne, D. Pollard, S. F. Price, A. Quiquet, T. J. Reerink, R. Reese, C. B. Rodehacke, N.-J. Schlegel, A. Shepherd, S. Sun, J. Sutter, J. Van Breedam, R. S. W. van de Wal, R. Winkelmann, T. Zhang
Publikováno v:
The Cryosphere, Vol 13, Pp 1441-1471 (2019)
Ice sheet numerical modeling is an important tool to estimate the dynamic contribution of the Antarctic ice sheet to sea level rise over the coming centuries. The influence of initial conditions on ice sheet model simulations, however, is still uncle
Externí odkaz:
https://doaj.org/article/bb75ff064b7840149a9727ba792420c6