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Evidence for Atlantic Ocean forcing the atmosphere and the negative role of model bias

Evidence for Atlantic Ocean forcing the atmosphere and the negative role of model bias
Evidence for Atlantic Ocean forcing the atmosphere and the negative role of model bias
There is agreement on how the North Atlantic Oscillation forces the Atlantic Meridional Overturning Circulation, but the existence of a reversed interaction is widely disputed. Here, we investigate this type of ocean forcing the atmosphere by analysing several high- and low-resolution coupled climate models, ocean observations and reanalyses products of ocean and atmosphere. We find that in observations and about 50% of the coupled climate models, an ocean-forced negative North Atlantic Oscillation occurs at a lag of 5 years after the Atlantic Meridional Overturning Circulation peaks. Climate models with a strong cold temperature bias in the subpolar gyre and a positive sea-ice cover bias in the Atlantic and Arctic Ocean are unable to correctly simulate the heat flux pattern, resulting from the northward propagation of warm ocean temperatures, that forces the atmosphere. Efforts to remove this bias could therefore lead to substantial improvement in current decadal prediction systems.
Haarsma, Reindert J.
52de705c-7df6-48c6-a891-99c8a01f4b09
Drijfhout, Sybren
a5c76079-179b-490c-93fe-fc0391aacf13
Haarsma, Reindert J.
52de705c-7df6-48c6-a891-99c8a01f4b09
Drijfhout, Sybren
a5c76079-179b-490c-93fe-fc0391aacf13

Haarsma, Reindert J. and Drijfhout, Sybren (2025) Evidence for Atlantic Ocean forcing the atmosphere and the negative role of model bias. Communications Earth & Environment, 6 (1), [125]. (doi:10.1038/s43247-025-02123-5).

Record type: Article

Abstract

There is agreement on how the North Atlantic Oscillation forces the Atlantic Meridional Overturning Circulation, but the existence of a reversed interaction is widely disputed. Here, we investigate this type of ocean forcing the atmosphere by analysing several high- and low-resolution coupled climate models, ocean observations and reanalyses products of ocean and atmosphere. We find that in observations and about 50% of the coupled climate models, an ocean-forced negative North Atlantic Oscillation occurs at a lag of 5 years after the Atlantic Meridional Overturning Circulation peaks. Climate models with a strong cold temperature bias in the subpolar gyre and a positive sea-ice cover bias in the Atlantic and Arctic Ocean are unable to correctly simulate the heat flux pattern, resulting from the northward propagation of warm ocean temperatures, that forces the atmosphere. Efforts to remove this bias could therefore lead to substantial improvement in current decadal prediction systems.

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e-pub ahead of print date: 20 February 2025

Identifiers

Local EPrints ID: 503536
URI: http://eprints.soton.ac.uk/id/eprint/503536
PURE UUID: 39205fef-f181-4a77-b303-b46370a3435c
ORCID for Sybren Drijfhout: ORCID iD orcid.org/0000-0001-5325-7350

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Date deposited: 05 Aug 2025 16:32
Last modified: 22 Aug 2025 02:07

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Author: Reindert J. Haarsma

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