Use of CMIP Atmospheric Boundary Conditions with ISMs
Dynamical ice sheet models are being used in simulations of future sea level change resulting from changing glacier mass. One of the difficulties in doing so are the input conditions obtained from earth system models. These inputs can be of coarse spatial resolution, and may not represent surface me...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20170012230 2023-05-15T16:40:28+02:00 Use of CMIP Atmospheric Boundary Conditions with ISMs Cullather, Richard Nowicki, Sophie Unclassified, Unlimited, Publicly available December 10, 2017 application/pdf http://hdl.handle.net/2060/20170012230 unknown Document ID: 20170012230 http://hdl.handle.net/2060/20170012230 Copyright, Public use permitted CASI Meteorology and Climatology GSFC-E-DAA-TN50498 AGU Fall Meeting 2017; 11-15 Dec. 2017; New Orleans, LA; United States|ISMIP6 (Ice Sheet Model Intercomparison for CMIP6 (Coupled Model Intercomparison Project Phase 6)) Pre-AGU workshop; 10 Dec. 2017; New Orleans, LA; United States 2017 ftnasantrs 2019-07-20T23:22:28Z Dynamical ice sheet models are being used in simulations of future sea level change resulting from changing glacier mass. One of the difficulties in doing so are the input conditions obtained from earth system models. These inputs can be of coarse spatial resolution, and may not represent surface melt in a future climate. I review various methods for overcoming this with the aim of promoting discussion among modelers. Other/Unknown Material Ice Sheet NASA Technical Reports Server (NTRS) |
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Open Polar |
collection |
NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Meteorology and Climatology |
spellingShingle |
Meteorology and Climatology Cullather, Richard Nowicki, Sophie Use of CMIP Atmospheric Boundary Conditions with ISMs |
topic_facet |
Meteorology and Climatology |
description |
Dynamical ice sheet models are being used in simulations of future sea level change resulting from changing glacier mass. One of the difficulties in doing so are the input conditions obtained from earth system models. These inputs can be of coarse spatial resolution, and may not represent surface melt in a future climate. I review various methods for overcoming this with the aim of promoting discussion among modelers. |
format |
Other/Unknown Material |
author |
Cullather, Richard Nowicki, Sophie |
author_facet |
Cullather, Richard Nowicki, Sophie |
author_sort |
Cullather, Richard |
title |
Use of CMIP Atmospheric Boundary Conditions with ISMs |
title_short |
Use of CMIP Atmospheric Boundary Conditions with ISMs |
title_full |
Use of CMIP Atmospheric Boundary Conditions with ISMs |
title_fullStr |
Use of CMIP Atmospheric Boundary Conditions with ISMs |
title_full_unstemmed |
Use of CMIP Atmospheric Boundary Conditions with ISMs |
title_sort |
use of cmip atmospheric boundary conditions with isms |
publishDate |
2017 |
url |
http://hdl.handle.net/2060/20170012230 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
CASI |
op_relation |
Document ID: 20170012230 http://hdl.handle.net/2060/20170012230 |
op_rights |
Copyright, Public use permitted |
_version_ |
1766030873851854848 |