Back to Search Start Over

An assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part II: Liquid freshwater

Authors :
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.
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.
Source :
Ocean Modelling (1463-5003) (Elsevier Sci Ltd), 2016-03 , Vol. 99 , P. 86-109
Publication Year :
2016

Abstract

The Arctic Ocean simulated in 14 global ocean-sea ice models in the framework of the Coordinated Ocean-ice Reference Experiments, phase II (CORE-II) is analyzed in this study. The focus is on the Arctic liquid freshwater (FW) sources and freshwater content (FWC). The models agree on the interannual variability of liquid FW transport at the gateways where the ocean volume transport determines the FW transport variability. The variation of liquid FWC is induced by both the surface FW flux (associated with sea ice production) and lateral liquid FW transport, which are in phase when averaged on decadal time scales. The liquid FWC shows an increase starting from the mid-1990s, caused by the reduction of both sea ice formation and liquid FW export, with the former being more significant in most of the models. The mean state of the FW budget is less consistently simulated than the temporal variability. The model ensemble means of liquid FW transport through the Arctic gateways compare well with observations. On average, the models have too high mean FWC, weaker upward trends of FWC in the recent decade than the observation, and low consistency in the temporal variation of FWC spatial distribution, which needs to be further explored for the purpose of model development.

Details

Database :
OAIster
Journal :
Ocean Modelling (1463-5003) (Elsevier Sci Ltd), 2016-03 , Vol. 99 , P. 86-109
Notes :
application/pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1253160423
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.1016.j.ocemod.2015.12.009