- Home
- Search Results
- Page 1 of 1
Search for: All records
-
Total Resources3
- Resource Type
-
10020
- Availability
-
30
- Author / Contributor
- Filter by Author / Creator
-
-
Stroeve, J. (2)
-
Andrews, M. (1)
-
Ayotte, K. (1)
-
Ballinger, T. J. (1)
-
Bhatt, U. S. (1)
-
Carmack, E. C. (1)
-
Chen, H. W. (1)
-
Cohen, J. (1)
-
Coumou, D. (1)
-
Demir, O. (1)
-
Fajber, R. (1)
-
Feldstein, S. (1)
-
Francis, J. (1)
-
Gille, S. T. (1)
-
Gu, H. (1)
-
Handorf, D. (1)
-
Henderson, G. (1)
-
Hendricks, S. (1)
-
Huntemann, M. (1)
-
Ionita, M. (1)
-
- Filter by Editor
-
-
& Spizer, S. M. (0)
-
& . Spizer, S. (0)
-
& Ahn, J. (0)
-
& Bateiha, S. (0)
-
& Bosch, N. (0)
-
& Brennan K. (0)
-
& Brennan, K. (0)
-
& Chen, B. (0)
-
& Chen, Bodong (0)
-
& Drown, S. (0)
-
& Ferretti, F. (0)
-
& Higgins, A. (0)
-
& J. Peters (0)
-
& Kali, Y. (0)
-
& Ruiz-Arias, P.M. (0)
-
& S. Spitzer (0)
-
& Sahin. I. (0)
-
& Spitzer, S. (0)
-
& Spitzer, S.M. (0)
-
(submitted - in Review for IEEE ICASSP-2024) (0)
-
-
Have feedback or suggestions for a way to improve these results?
!
Note: When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external site maintained by the publisher.
Some full text articles may not yet be available without a charge during the embargo (administrative interval).
What is a DOI Number?
Some links on this page may take you to non-federal websites. Their policies may differ from this site.
-
Rosenblum, E. ; Fajber, R. ; Stroeve, J. C. ; Gille, S. T. ; Tremblay, L. B. ; Carmack, E. C. ( , Geophysical Research Letters)
Abstract The Canada Basin has exhibited a significant trend toward a fresher surface layer and thus a more stratified upper‐ocean over the past three decades. State‐of‐the‐art ice‐ocean models, by contrast, tend to simulate a surface layer that is saltier and less stratified than observed. Here, we examine decadal changes to seasonal processes that may contribute to this wide‐reaching model bias using climate model simulations from the Community Earth System Model and below‐ice observations from the Arctic Ice Dynamics Joint Experiment in 1975 and Ice Tethered Profilers in 2006–2012. In contrast to the observations, the models simulate salinity profiles that show relatively little variation between 1975 and 2012. We demonstrate that this bias can be mainly attributed to unrealistically deep vertical mixing in the model, creating a surface layer that is saltier than observed. The results provide insight for climate model improvement with broad implications for Arctic sea ice and ecosystem dynamics.
-
Cohen, J. ; Zhang, X. ; Francis, J. ; Jung, T. ; Kwok, R. ; Overland, J. ; Ballinger, T. J. ; Bhatt, U. S. ; Chen, H. W. ; Coumou, D. ; et al ( , Nature Climate Change)