Sea Ice Effects on the Sensitivity of the Thermohaline Circulation

PDF: http://data.dhkim.info/monograph/JCLI/i1520-0442-011-11-2789.pdf

doi: 10.1175/1520-0442(1998)011<2789:SIEOTS>2.0.CO;2
Journal of Climate: Vol. 11, No. 11, pp. 2789–2803.

Sea Ice Effects on the Sensitivity of the Thermohaline Circulation*
Gerrit Lohmann and Rüdiger Gerdes

Alfred-Wegener-Institute for Polar and Marine Research, Bremerhaven, Germany


(Manuscript received 18 June 1996, 8 January 1998)


ABSTRACT

The authors investigate the sensitivity of the thermohaline circulation (THC) with respect to a subpolar salinity perturbation. Such perturbation simulates a freshwater release caused by retreating glaciers or anomalous sea ice. The feedback mechanisms amplifying or damping the initial anomaly are analyzed in the coupled ocean–atmosphere–sea ice model. Their understanding is essential for modeling climate variability on decadal and longer timescales.

A 3D ocean circulation model is coupled to an atmospheric energy balance and a thermodynamic sea ice model. The perturbation in the North Atlantic’s subpolar salinity causes a cessation of deep convection and a climate state with decreased oceanic heat transport, decreased high-latitude atmospheric temperature, and larger sea ice extent. The sea ice isolates the atmosphere from the warmer ocean, reducing the heat flux and thus the vertical mixing in the ocean. This change in the local buoyancy flux weakens the large-scale circulation. High-latitude cooling cannot compensate for the freshening since the ocean temperature cannot fall below the freezing point. Because deep convection is suppressed where sea ice is present, North Atlantic deep water formation is rather sensitive to the formation of sea ice. The insulating effect of sea ice is more important than its impact on salinity in our experiments. Different types of boundary conditions are used to isolate relevant feedback processes. The stability of the THC depends crucially on the atmospheric model component. Active atmospheric heat transport allows continued deep water formation because the sea ice margin is shifted poleward.