Sensitivity of open-water ice growth and ice concentration evolution in a coupled atmosphere-ocean-sea ice model

被引:13
作者
Shi, Xiaoxu [1 ]
Lohmann, Gerrit [1 ]
机构
[1] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bussestr 24, D-27570 Bremerhaven, Germany
关键词
Sea ice concentration; Sea ice transport; AMOC; Lead closing parameter; MERIDIONAL OVERTURNING CIRCULATION; GREASE-ICE; PART I; THERMOHALINE CIRCULATION; THICKNESS DISTRIBUTION; DECADAL TRENDS; GLOBAL CLIMATE; ARCTIC-OCEAN; PARAMETERIZATION; SYSTEM;
D O I
10.1016/j.dynatmoce.2017.05.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A coupled atmosphere-ocean-sea ice model is applied to investigate to what degree the area-thickness distribution of new ice formed in open water affects the ice and ocean properties. Two sensitivity experiments are performed which modify the horizontal-to-vertical aspect ratio of open-water ice growth. The resulting changes in the Arctic sea-ice concentration strongly affect the surface albedo, the ocean heat release to the atmosphere, and the sea-ice production. The changes are further amplified through a positive feedback mechanism among the Arctic sea ice, the Atlantic Meridional Overturning Circulation (AMOC), and the surface air temperature in the Arctic, as the Fram Strait sea ice import influences the freshwater budget in the North Atlantic Ocean. Anomalies in sea-ice transport lead to changes in sea surface properties of the North Atlantic and the strength of AMOC. For the Southern Ocean, the most pronounced change is a warming along the Antarctic Circumpolar Current (ACC), owing to the interhemispheric bipolar seasaw linked to AMOC weakening. Another insight of this study lies on the improvement of our climate model. The ocean component FESOM is a newly developed ocean-sea ice model with an unstructured mesh and multi-resolution. We find that the subpolar sea-ice boundary in the Northern Hemisphere can be improved by tuning the process of open-water ice growth, which strongly influences the sea ice concentration in the marginal ice zone, the North Atlantic circulation, salinity and Arctic sea ice volume. Since the distribution of new ice on open water relies on many uncertain parameters and the knowledge of the detailed processes is currently too crude, it is a challenge to implement the processes realistically into models. Based on our sensitivity experiments, we conclude a pronounced uncertainty related to open-water sea ice growth which could significantly affect the climate system sensitivity. (C) 2017 The Author(s). Published by Elsevier B.V.
引用
收藏
页码:10 / 30
页数:21
相关论文
共 105 条
  • [1] THE ROLE OF SEA ICE AND OTHER FRESH-WATER IN THE ARCTIC CIRCULATION
    AAGAARD, K
    CARMACK, EC
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1989, 94 (C10) : 14485 - 14498
  • [2] Evolution of new ice and turbulent fluxes over freezing winter leads
    Alam, A
    Curry, JA
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1998, 103 (C8): : 15783 - 15802
  • [3] [Anonymous], 1980, REV GEOPHYS, V18, P525
  • [4] [Anonymous], 1986, SURFACE HEAT MASS BA
  • [5] [Anonymous], 2013, Contribution of working group i to the fifth assessment report of the intergovernmental panel on climate change
  • [6] [Anonymous], GEOSCI MODEL DEV DIS
  • [7] Bengtsson L, 2004, J CLIMATE, V17, P4045, DOI 10.1175/1520-0442(2004)017<4045:TETWIT>2.0.CO
  • [8] 2
  • [9] LONG-TERM VARIATIONS OF CALORIC INSOLATION RESULTING FROM EARTHS ORBITAL ELEMENTS
    BERGER, AL
    [J]. QUATERNARY RESEARCH, 1978, 9 (02) : 139 - 167
  • [10] Polynya flux model solutions incorporating a parameterization for the collection thickness of consolidated new ice
    Biggs, NRT
    Maqueda, MAM
    Willmott, AJ
    [J]. JOURNAL OF FLUID MECHANICS, 2000, 408 : 179 - 204