FN Archimer Export Format
PT J
TI An assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part I: Sea ice and solid freshwater
BT 
AF WANG, Qiang
   ILICAK, Mehmet
   GERDES, Ruediger
   DRANGE, Helge
   AKSENOV, Yevgeny
   BAILEY, David A.
   BENTSEN, Mats
   BIASTOCH, Arne
   BOZEC, Alexandra
   BOENING, Claus
   CASSOU, Christophe
   CHASSIGNET, Eric
   COWARD, Andrew C.
   CURRY, Beth
   DANABASOGLU, Gokhan
   DANILOV, Sergey
   FERNANDEZ, Elodie
   FOGLI, Pier Giuseppe
   FUJII, Yosuke
   GRIFFIES, Stephen M.
   IOVINO, Doroteaciro
   JAHN, Alexandra
   JUNG, Thomas
   LARGE, William G.
   LEE, Craig
   LIQUE, Camille
   LU, Jianhua
   MASINA, Simona
   NURSER, A. J. George
   RABE, Benjamin
   ROTH, Christina
   SALAS Y MELIA, David
   SAMUELS, Bonita L.
   SPENCE, Paul
   TSUJINO, Hiroyuki
   VALCKE, Sophie
   VOLDOIRE, Aurore
   WANG, Xuezhu
   YEAGER, Steve G.
AS 1:1;2:2;3:1;4:3;5:4;6:5;7:2;8:6;9:7;10:6;11:8;12:7;13:4;14:9;15:5;16:1;17:8;18:10;19:11;20:12;21:10;22:5,13,14;23:15;24:5;25:9;26:16,17;27:7;28:10,21;29:4;30:1;31:6;32:18;33:12;34:19,20;35:11;36:8;37:18;38:1;39:5;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;25:;26:PDG-ODE-LOPS-OH;27:;28:;29:;30:;31:;32:;33:;34:;35:;36:;37:;38:;39:;
C1 Helmholtz Ctr Polar & Marine Res AWI, Bremerhaven, Germany.
   Uni Res Ltd, Bergen, Norway.
   Univ Bergen, Bergen, Norway.
   NOC, Southampton SO14 3ZH, Hants, England.
   Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA.
   GEOMAR Helmholtz Ctr Ocean Res, Kiel, Germany.
   Florida State Univ, COAPS, Tallahassee, FL 32306 USA.
   CERFACS, Toulouse, France.
   Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA.
   Ctr Euromediterrarteo Cambiamenti Climat CMCC, Bologna, Italy.
   Japan Meteorol Agcy, MRI, Tsukuba, Ibaraki, Japan.
   NOAA, GFDL, Princeton, NJ USA.
   Univ Colorado, Dept Atmospher & Ocean Sci, Boulder, CO 80309 USA.
   Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80309 USA.
   Univ Bremen, Inst Environm Phys, D-28359 Bremen, Germany.
   Univ Oxford, Dept Earth Sci, Oxford OX1 3PR, England.
   IFREMER, Ctr Brest, Lab Phys Oceans, Plouzane, France.
   CNRM, Toulouse, France.
   Univ New S Wales, Climate Change Res Ctr, Sydney, NSW, Australia.
   Univ New S Wales, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia.
   INGV, Bologna, Italy.
C2 INST A WEGENER, GERMANY
   UNI RES BERGEN, NORWAY
   UNIV BERGEN, NORWAY
   NOC, UK
   NCAR NATL CTR ATMOSPHER RES, USA
   GEOMAR HELMHOLTZ CTR OCEAN RES, GERMANY
   UNIV FLORIDA STATE, USA
   CERFACS, FRANCE
   UNIV WASHINGTON, USA
   CMCC, ITALY
   JAPAN METEOROL AGCY, JAPAN
   NOAA, USA
   UNIV COLORADO, USA
   UNIV COLORADO, USA
   UNIV BREMEN, GERMANY
   UNIV OXFORD, UK
   IFREMER, FRANCE
   CNRM (METEO FRANCE), FRANCE
   UNIV NEW S WALES, AUSTRALIA
   UNIV NEW S WALES, AUSTRALIA
   INGV, ITALY
SI BREST
SE PDG-ODE-LOPS-OH
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-europe
   copubli-int-hors-europe
IF 3.341
TC 63
UR https://archimer.ifremer.fr/doc/00307/41812/84134.pdf
LA English
DT Article
DE ;Arctic Ocean;Sea ice;Freshwater;CORE II atmospheric forcing
AB The Arctic Ocean simulated in fourteen global ocean-sea ice models in the framework of the Coordinated Ocean-ice Reference Experiments, phase II (CORE II) is analyzed. The focus is on the Arctic sea ice extent, the solid freshwater (FW) sources and solid freshwater content (FWC). Available observations are used for model evaluation. The variability of sea ice extent and solid FW budget is more consistently reproduced than their mean state in the models. The descending trend of September sea ice extent is well simulated in terms of the model ensemble mean. Models overestimating sea ice thickness tend to underestimate the descending trend of September sea ice extent. The models underestimate the observed sea ice thinning trend by a factor of two. When averaged on decadal time scales, the variation of Arctic solid FWC is contributed by those of both sea ice production and sea ice transport, which are out of phase in time. The solid FWC decreased in the recent decades, caused mainly by the reduction in sea ice thickness. The models did not simulate the acceleration of sea ice thickness decline, leading to an underestimation of solid FWC trend after 2000. The common model behavior, including the tendency to underestimate the trend of sea ice thickness and March sea ice extent, remains to be improved
PY 2016
PD MAR
SO Ocean Modelling
SN 1463-5003
PU Elsevier Sci Ltd
VL 99
UT 000371792800008
BP 110
EP 132
DI 10.1016/j.ocemod.2015.12.008
ID 41812
ER

EF