論文

査読有り 本文へのリンクあり 国際共著 国際誌
2021年8月

Future sea level change under Coupled Model Intercomparison Project Phase 5 and Phase 6 scenarios from the Greenland and Antarctic ice sheets

Geophysical Research Letters
  • Antony J. Payne
  • Sophie Nowicki
  • Ayako Abe-Ouchi
  • Cecile Agosta
  • Patrick Alexander
  • Torsten Albrecht
  • Xylar Asay-Davis
  • Andy Aschwanden
  • Alice Barthel
  • Thomas J. Bracegirdle
  • Reinhard Calov
  • Christopher Chambers
  • Youngmin Choi
  • Richard Cullather
  • Joshua Cuzzone
  • Christophe Dumas
  • Tamsin L. Edwards
  • Denis Felikson
  • Xavier Fettweis
  • Benjamin K. Galton-Fenzi
  • Heiko Goelzer
  • Rupert Gladstone
  • Nicholas R. Golledge
  • Jonathan M. Gregory
  • Ralf Greve
  • Tore Hattermann
  • Matthew J. Hoffman
  • Angelika Humbert
  • Philippe Huybrechts
  • Nicolas C. Jourdain
  • Thomas Kleiner
  • Peter Kuipers Munneke
  • Eric Larour
  • Sebastien Le Clec'h
  • Victoria Lee
  • Gunter Leguy
  • William H. Lipscomb
  • Christopher M. Little
  • Daniel P. Lowry
  • Mathieu Morlighem
  • Isabel Nias
  • Frank Pattyn
  • Tyler Pelle
  • Stephen F. Price
  • Aurelien Quiquet
  • Ronja Reese
  • Martin Rueckamp
  • Nicole-Jeanne Schlegel
  • Helene Seroussi
  • Andrew Shepherd
  • Erika Simon
  • Donald Slater
  • Robin S. Smith
  • Fiammetta Straneo
  • Sainan Sun
  • Lev Tarasov
  • Luke D. Trusel
  • Jonas Van Breedam
  • Roderik van de Wal
  • Michiel van den Broeke
  • Ricarda Winkelmann
  • Chen Zhao
  • Tong Zhang
  • Thomas Zwinger
  • 全て表示

48
16
開始ページ
e2020GL091741
終了ページ
記述言語
英語
掲載種別
研究論文(学術雑誌)
DOI
10.1029/2020GL091741
出版者・発行元
American Geophysical Union

Projections of the sea level contribution from the Greenland and Antarctic ice sheets (GrIS and AIS) rely on atmospheric and oceanic drivers obtained from climate models. The Earth System Models participating in the Coupled Model Intercomparison Project phase 6 (CMIP6) generally project greater future warming compared with the previous Coupled Model Intercomparison Project phase 5 (CMIP5) effort. Here we use four CMIP6 models and a selection of CMIP5 models to force multiple ice sheet models as part of the Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6). We find that the projected sea level contribution at 2100 from the ice sheet model ensemble under the CMIP6 scenarios falls within the CMIP5 range for the Antarctic ice sheet but is significantly increased for Greenland. Warmer atmosphere in CMIP6 models results in higher Greenland mass loss due to surface melt. For Antarctica, CMIP6 forcing is similar to CMIP5 and mass gain from increased snowfall counteracts increased loss due to ocean warming.

リンク情報
DOI
https://doi.org/10.1029/2020GL091741 本文へのリンクあり
Web of Science
https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=JSTA_CEL&SrcApp=J_Gate_JST&DestLinkType=FullRecord&KeyUT=WOS:000688759800065&DestApp=WOS_CPL
ID情報
  • DOI : 10.1029/2020GL091741
  • ISSN : 0094-8276
  • eISSN : 1944-8007
  • Web of Science ID : WOS:000688759800065

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