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245 00 |a IPCC climate models do not capture Arctic sea ice drift acceleration |h [electronic resource] |b Consequences in terms of projected sea ice thinning and decline |y English.
260        |a [S.l.] : |b American Geophysical Union, |c 2011-09-29.
490        |a Journal of Geophysical Research Volume 116.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a IPCC climate models underestimate the decrease of the Arctic sea ice extent. The recent Arctic sea ice decline is also characterized by a rapid thinning and by an increase of sea ice kinematics (velocities and deformation rates), with both processes being coupled through positive feedbacks. In this study we show that IPCC climate models underestimate the observed thinning trend by a factor of almost 4 on average and fail to capture the associated accelerated motion. The coupling between the ice state (thickness and concentration) and ice velocity is unexpectedly weak in most models. In particular, sea ice drifts faster during the months when it is thick and packed than when it is thin, contrary to what is observed; also models with larger long‐term thinning trends do not show higher drift acceleration. This weak coupling behavior (1) suggests that the positive feedbacks mentioned above are underestimated and (2) can partly explain the models’ underestimation of the recent sea ice area, thickness, and velocity trends. Due partly to this weak coupling, ice export does not play an important role in the simulated negative balance of Arctic sea ice mass between 1950 and 2050. If we assume a positive trend on ice speeds at straits equivalent to the one observed since 1979 within the Arctic basin, first‐order estimations give shrinking and thinning trends that become significantly closer to the observations.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a climate change.
650        |a sea ice.
650        |a kinematics.
651        |a Arctic Ocean Region.
700        |a P. Rampal.
700        |a J. Weiss.
700        |a C. Dubois.
700        |a J.M. Campin.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15050355/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/05/03/55/00001/FI15050355_thm.jpg
997        |a Sea Level Rise


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