Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
Exploring the impact of atmospheric forcing and basal drag on the Antarctic Ice Sheet under Last Glacial Maximum conditions ; volume:15 ; number:1 ; year:2021 ; pages:215-231
The Cryosphere ; 15, Heft 1 (2021), 215-231
- Creator
-
Blasco, Javier
Alvarez-Solas, Jorge
Robinson, Alexander
Montoya, Marisa
- DOI
-
10.5194/tc-15-215-2021
- URN
-
urn:nbn:de:101:1-2021012104203387477930
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
15.08.2025, 7:28 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Blasco, Javier
- Alvarez-Solas, Jorge
- Robinson, Alexander
- Montoya, Marisa
Other Objects (12)
Exploring the impact of atmospheric forcing and basal boundary conditions on the simulation of the Antarctic ice sheet at the Last Glacial Maximum
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Incorporating modelled subglacial hydrology into inversions for basal drag
Improved basal drag of the West Antarctic Ice Sheet from L-curve analysis of inverse models utilizing subglacial hydrology simulations
A Last Glacial Maximum forcing dataset for ocean modelling
A Last Glacial Maximum forcing dataset for ocean modelling
Astronomical forcing and mathematical theory of glacial-interglacial cycles
Basal Water Storage Variations beneath Antarctic Ice Sheet
Tropical and mid-latitude forcing of continental Antarctic temperatures
Pleistocene glacial variability as a chaotic response to obliquity forcing
Volcanic forcing and climate variations during the last glacial period
Exploring the impact of atmospheric forcing and basal boundary conditions on the simulation of the Antarctic ice sheet at the Last Glacial Maximum
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Incorporating modelled subglacial hydrology into inversions for basal drag
Improved basal drag of the West Antarctic Ice Sheet from L-curve analysis of inverse models utilizing subglacial hydrology simulations
A Last Glacial Maximum forcing dataset for ocean modelling
A Last Glacial Maximum forcing dataset for ocean modelling
Astronomical forcing and mathematical theory of glacial-interglacial cycles
Basal Water Storage Variations beneath Antarctic Ice Sheet
Tropical and mid-latitude forcing of continental Antarctic temperatures
Pleistocene glacial variability as a chaotic response to obliquity forcing
Volcanic forcing and climate variations during the last glacial period
Exploring the impact of atmospheric forcing and basal boundary conditions on the simulation of the Antarctic ice sheet at the Last Glacial Maximum
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Subglacial hydrology modulates basal sliding response of the Antarctic ice sheet to climate forcing
Incorporating modelled subglacial hydrology into inversions for basal drag
Improved basal drag of the West Antarctic Ice Sheet from L-curve analysis of inverse models utilizing subglacial hydrology simulations
A Last Glacial Maximum forcing dataset for ocean modelling
A Last Glacial Maximum forcing dataset for ocean modelling
Astronomical forcing and mathematical theory of glacial-interglacial cycles
Basal Water Storage Variations beneath Antarctic Ice Sheet
Tropical and mid-latitude forcing of continental Antarctic temperatures
Pleistocene glacial variability as a chaotic response to obliquity forcing