The sensitivity of a coupled climate model to its ocean component

Megann, A.P. ORCID: https://orcid.org/0000-0003-0975-6317; New, A.L. ORCID: https://orcid.org/0000-0002-3159-8872; Blaker, A.T. ORCID: https://orcid.org/0000-0001-5454-0131; Sinha, B.. 2010 The sensitivity of a coupled climate model to its ocean component. Journal of Climate, 23 (19). 5126-5150. 10.1175/2010JCLI3394.1

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Abstract/Summary

The control climates of two coupled climate models are intercompared. The first is the third climate configuration of the Met Office Unified Model (HadCM3), while the second, the Coupled Hadley–Isopycnic Model Experiment (CHIME), is identical to the first except for the replacement of its ocean component by the Hybrid-Coordinate Ocean Model (HYCOM). Both models possess realistic and similar ocean heat transports and overturning circulation. However, substantial differences in the vertical structure of the two ocean components are observed, some of which are directly attributed to their different vertical coordinate systems. In particular, the sea surface temperature (SST) in CHIME is biased warm almost everywhere, particularly in the North Atlantic subpolar gyre, in contrast to HadCM3, which is biased cold except in the Southern Ocean. Whereas the HadCM3 ocean warms from just below the surface down to 1000-m depth, a similar warming in CHIME is more pronounced but shallower and confined to the upper 400 m, with cooling below this. This is particularly apparent in the subtropical thermoclines, which become more diffuse in HadCM3, but sharper in CHIME. This is interpreted as resulting from a more rigorously controlled diapycnal mixing in the interior isopycnic ocean in CHIME. Lower interior mixing is also apparent in the better representation and maintenance of key water masses in CHIME, such as Subantarctic Mode Water, Antarctic Intermediate Water, and North Atlantic Deep Water. Finally, the North Pacific SST cold error in HadCM3 is absent in CHIME, and may be related to a difference in the separation position of the Kuroshio. Disadvantages of CHIME include a nonconservation of heat equivalent to 0.5 W m−2 globally, and a warming and salinification of the northwestern Atlantic.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1175/2010JCLI3394.1
ISSN:	0894-8755
Date made live:	02 Nov 2010 11:29 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/266795

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1175/2010JCLI3394.1

ISSN:

0894-8755

Date made live:

02 Nov 2010 11:29 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/266795