The impact of salinity perturbations on the future uptake of heat by the Atlantic Ocean

Smith, R. S. ORCID: https://orcid.org/0000-0001-7479-7778, Sutton, R. ORCID: https://orcid.org/0000-0001-8345-8583 and Gregory, J. M. ORCID: https://orcid.org/0000-0003-1296-8644 (2014) The impact of salinity perturbations on the future uptake of heat by the Atlantic Ocean. Geophysical Research Letters, 41 (24). pp. 9072-9079. ISSN 0094-8276 doi: 10.1002/2014GL062169

Abstract/Summary

Anthropogenic ocean heat uptake is a key factor in determining climate change and sea-level rise. There is considerable uncertainty in projections of freshwater forcing of the ocean, with the potential to influence ocean heat uptake. We investigatethis by adding either -0.1 Sv or +0.1 Sv freshwater to the Atlantic in global climate model simulations, simultaneously imposing an atmospheric CO2 increase. The resulting changes in the Atlantic meridional overturning circulation are roughly equal and opposite (±2Sv). The impact of the perturbation on ocean heat content is more complex, although it is relatively small (~5%) compared to the total anthropogenic heat uptake. Several competing processes either accelerate or retard warming at different depths. Whilst positive freshwater perturbations cause an overall heating of the Atlantic, negative perturbations produce insignificant net changes in heat content. The processes active in our model appear robust, although their net result is likely model- and experiment-dependent.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/38428
Item Type	Article
Refereed	Yes
Divisions	Science > School of Mathematical, Physical and Computational Sciences > NCAS Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Uncontrolled Keywords	Ocean heat content;Atlantic;Overturning circulation;Climate change
Publisher	American Geophysical Union
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