Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica-Reference-Cited by-同舟云学术

Comparing Glacial‐Geological Evidence and Model Simulations of Ice Sheet Change since the Last Glacial Period in the Amundsen Sea Sector of Antarctica

Published:2021-06 Issue:6 Volume:126 Page:
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Johnson Joanne S.¹^ORCID,Pollard David²^ORCID,Whitehouse Pippa L.³^ORCID,Roberts Stephen J.¹^ORCID,Rood Dylan H.⁴^ORCID,Schaefer Joerg M.⁵^ORCID

Affiliation:

1. British Antarctic Survey Cambridge UK

2. Earth and Environmental Systems Institute Pennsylvania State University University Park PA USA

3. Department of Geography Durham University Durham UK

4. Department of Earth Science & Engineering Imperial College London London UK

5. Lamont‐Doherty Earth Observatory Columbia University Palisades NY USA

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020JF005827

Reference105 articles.

1. Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 1: Boundary conditions and climatic forcing

2. Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM) – Part 2: Parameter ensemble analysis

3. Ocean-forced evolution of the Amundsen Sea catchment, West Antarctica, by 2100

4. Response of the East Antarctica ice sheet to sea-level rise

5. S -velocity model and inferred Moho topography beneath the Antarctic Plate from Rayleigh waves

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