The Importance of a Properly Represented Stratosphere for Northern Hemisphere Surface Variability in the Atmosphere and the Ocean

Major sudden stratospheric warmings (SSWs) are extreme events during boreal winter, which not only impact tropospheric weather up to three months but also can influence oceanic variability through wind stress and heat flux anomalies. In the North Atlantic region, SSWs have the potential to modulate...

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Bibliographic Details
Published in:Journal of Climate
Main Authors: Haase, Sabine, Matthes, Katja, Latif, Mojib, Omrani, Nour-Eddine
Format: Article in Journal/Newspaper
Language:English
Published: AMS (American Meteorological Society) 2018
Subjects:
Pacific
aleutian low
Labrador Sea
North Atlantic
Online Access:https://oceanrep.geomar.de/id/eprint/43989/
https://oceanrep.geomar.de/id/eprint/43989/1/jcli-d-17-0520.1.pdf
https://oceanrep.geomar.de/id/eprint/43989/2/10.1175_JCLI-D-17-0520.s1.pdf
https://doi.org/10.1175/JCLI-D-17-0520.1
Description
Summary:Major sudden stratospheric warmings (SSWs) are extreme events during boreal winter, which not only impact tropospheric weather up to three months but also can influence oceanic variability through wind stress and heat flux anomalies. In the North Atlantic region, SSWs have the potential to modulate deep convection in the Labrador Sea and thereby the strength of the Atlantic meridional overturning circulation. The impact of SSWs on the Northern Hemisphere surface climate is investigated in two coupled climate models: a stratosphere-resolving (high top) and a non-stratosphere-resolving (low top) model. In both configurations, a robust link between SSWs and a negative NAO is detected, which leads to shallower-than-normal North Atlantic mixed layer depth. The frequency of SSWs and the persistence of this link is better captured in the high-top model. Significant differences occur over the Pacific region, where an unrealistically persistent Aleutian low is observed in the low-top configuration. An overrepresentation of SSWs during El Nino conditions in the low-top model is the main cause for this artifact. Our results underline the importance of a proper representation of the stratosphere in a coupled climate model for a consistent surface response in both the atmosphere and the ocean, which, among others, may have implications for oceanic deep convection in the subpolar North Atlantic.

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