Zobrazeno 1 - 10
of 24
pro vyhledávání: '"A. G. Pauling"'
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
Autor:
Andrew G. Pauling, Cecilia M. Bitz
Publikováno v:
Earth's Future, Vol 9, Iss 10, Pp n/a-n/a (2021)
Abstract The projected decline in Arctic sea ice extent as the Earth warms in response to increased greenhouse gas concentrations will occur in conjunction with increased precipitation in the Arctic, and more of that precipitation is projected to fal
Externí odkaz:
https://doaj.org/article/053bcb333f7d40718904b8a7d5336183
Publikováno v:
Journal of Climate. :1-35
A hierarchy of general circulation models (GCMs) is used to investigate the linearity of the response of the climate system to changes in Antarctic topography. Experiments were conducted with a GCM with either a slab-ocean or fixed SSTs and sea ice,
Publikováno v:
Journal of Climate. :1-30
The West Antarctic Ice Sheet (WAIS) may have collapsed during the last interglacial period, between 132,000 and 116,000 years ago. The changes in topography resulting from WAIS collapse would be accompanied by significant changes in Antarctic surface
Publikováno v:
Geophysical Research Letters. 50
Autor:
Neil Swart, Torge Martin, Rebecca Beadling, Jia-Jia Chen, Mathew H. England, Riccardo Farneti, Stephen M. Griffies, Tore Hatterman, F. Alexander Haumann, Qian Li, John Marshall, Morven Muilwijk, Andrew G. Pauling, Ariaan Purich, Inga J. Smith, Max Thomas
As the climate warms, the grounded ice sheet and floating ice shelves surrounding Antarctica are losing mass at an increasing rate and injecting the resulting meltwater into the Southern Ocean. This freshwater input could feed back onto climate chang
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33ce4959a4109188dc19d98a8a002ccd
https://doi.org/10.5194/egusphere-2023-198
https://doi.org/10.5194/egusphere-2023-198
Publikováno v:
Geophysical Research Letters. 49
The West Antarctic Ice Sheet (WAIS) may have collapsed during the last interglacial period, between 132,000 and 116,000 years ago. The changes in topography resulting from WAIS collapse would be accompanied by significant changes in Antarctic surface
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e3b296c471dc963d4d41223e69a29cc
https://doi.org/10.5194/egusphere-egu22-8361
https://doi.org/10.5194/egusphere-egu22-8361
Autor:
Cecilia M. Bitz, Andrew G. Pauling
Publikováno v:
Earth's Future, Vol 9, Iss 10, Pp n/a-n/a (2021)
The projected decline in Arctic sea ice extent as the Earth warms in response to increased greenhouse gas concentrations will occur in conjunction with increased precipitation in the Arctic, and more of that precipitation is projected to fall as rain
Publikováno v:
Geophysical Research Letters. 48