Simulating Arctic Climate Warmth and Icefield Retreat in the Last Interglaciation
-
- Bette L. Otto-Bliesner
- Climate and Global Dynamics Division, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA.
-
- Shawn J. Marshall
- Climate and Global Dynamics Division, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA.
-
- Jonathan T. Overpeck
- Climate and Global Dynamics Division, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA.
-
- Gifford H. Miller
- Climate and Global Dynamics Division, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA.
-
- Aixue Hu
- Climate and Global Dynamics Division, National Center for Atmospheric Research (NCAR), Boulder, CO 80305, USA.
抄録
<jats:p>In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and paleoclimatic data to evaluate Northern Hemisphere high-latitude warming and its impact on Arctic icefields during the Last Interglaciation. Our simulated climate matches paleoclimatic observations of past warming, and the combination of physically based climate and ice-sheet modeling with ice-core constraints indicate that the Greenland Ice Sheet and other circum-Arctic ice fields likely contributed 2.2 to 3.4 meters of sea-level rise during the Last Interglaciation.</jats:p>
収録刊行物
-
- Science
-
Science 311 (5768), 1751-1753, 2006-03-24
American Association for the Advancement of Science (AAAS)
- Tweet
キーワード
詳細情報 詳細情報について
-
- CRID
- 1360292620790591744
-
- NII論文ID
- 80019245428
-
- ISSN
- 10959203
- 00368075
-
- データソース種別
-
- Crossref
- CiNii Articles