The amplification of Arctic terrestrial surface temperatures by reduced sea-ice extent during the Pliocene

Author:

Ballantyne Ashley P.,Axford Yarrow,Miller Gifford H.,Otto-Bliesner Bette L.,Rosenbloom Nan,White James W.C.

Funder

University of Colorado

U.S. National Science Foundation

National Science Foundation

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference61 articles.

1. Sea ice, high-latitude convection, and equable climates;Abbot;Geophysical Research Letters,2008

2. High-CO2 cloud radiative forcing feedback over both land and ocean in a global climate model;Abbot,2009

3. The importance of ice vertical resolution for Snowball climate and deglaciation;Abbot;Journal of Climate,2010

4. Arctic Climate Impact Assessment — Scientific Impact Report;ACIA,2005

5. Pliocene Arctic temperature constraints from the growth rings and isotopic composition of fossil larch;Ballantyne;Palaeogeography, Palaeoclimatology, Palaeoecology,2006

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