Historical Antarctic mean sea ice area, sea ice trends, and winds in CMIP5 simulations
Name
solomon 3 MahlsteinEtAlSeaIceJGR2013.pdf
Size
971.94 KB
Format
Adobe PDF
Checksum (MD5)
cca48619ce3316f7b41c0f62242741e2
Author(s) • •
Mahlstein, Irina
Gent, Peter R.
Solomon, Susan
Date Issued
June 2013
Journal
Journal of Geophysical Research: Atmospheres
Publisher
American Geophysical Union (AGU)
Citation
Mahlstein, Irina, Peter R. Gent, and Susan Solomon. “Historical Antarctic Mean Sea Ice Area, Sea Ice Trends, and Winds in CMIP5 Simulations.” Journal of Geophysical Research: Atmospheres 118, no. 11 (June 16, 2013): 5105–5110. © 2013 American Geophysical Union
Version
Final published version
Abstract
In contrast to Arctic sea ice, average Antarctic sea ice area is not retreating but has slowly increased since satellite measurements began in 1979. While most climate models from the Coupled Model Intercomparison Project Phase 5 (CMIP5) archive simulate a decrease in Antarctic sea ice area over the recent past, whether these models can be dismissed as being wrong depends on more than just the sign of change compared to observations. We show that internal sea ice variability is large in the Antarctic region, and both the observed and modeled trends may represent natural variations along with external forcing. While several models show a negative trend, only a few of them actually show a trend that is significant compared to their internal variability on the time scales of available observational data. Furthermore, the ability of the models to simulate the mean state of sea ice is also important. The representations of Antarctic sea ice in CMIP5 models have not improved compared to CMIP3 and show an unrealistic spread in the mean state that may influence future sea ice behavior. Finally, Antarctic climate and sea ice area will be affected not only by ocean and air temperature changes but also by changes in the winds. The majority of the CMIP5 models simulate a shift that is too weak compared to observations. Thus, this study identifies several foci for consideration in evaluating and improving the modeling of climate and climate change in the Antarctic region.
MIT Department
Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Terms of Use
Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
DOI of Published Version
https://doi.org/10.1002/jgrd.50443