Stratospheric winter climate response to ENSO in three chemistry-climate models

Three different chemistry‐climate models are compared with respect to their simulation of the stratospheric response to extreme cases of ENSO. Ensemble simulations of an unusually warm ENSO event (1940–1941) compared to a very cold event (1975–1976) reveal a weaker and warmer polar vortex in the Nor...

Full description

Saved in:
Bibliographic Details
Published in:Geophysical research letters 2008-07, Vol.35 (13), p.n/a
Main Authors: Fischer, A. M., Shindell, D. T., Winter, B., Bourqui, M. S., Faluvegi, G., Rozanov, E., Schraner, M., Brönnimann, S.
Format: Article
Language:English
Subjects:
CCM
Earth sciences
Earth, ocean, space
ENSO
Exact sciences and technology
Marine
stratosphere
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Three different chemistry‐climate models are compared with respect to their simulation of the stratospheric response to extreme cases of ENSO. Ensemble simulations of an unusually warm ENSO event (1940–1941) compared to a very cold event (1975–1976) reveal a weaker and warmer polar vortex in the Northern Hemisphere winter. This follows from anomalously propagating waves decelerating the zonal flow and strengthening the residual mean circulation. Models are in good agreement in simulating the observed (statistically reconstructed for the case 1941) flow in the lower stratosphere over the Pacific North American region, but less so over the North Atlantic European sector with insufficient reproduction of the wave structure. Modeled column ozone is reduced in the Tropics and increased on average in the northern extra tropics in accord with the general pattern seen in observations and in line with an intensification of the Brewer‐Dobson circulation.
ISSN:0094-8276
1944-8007
DOI:10.1029/2008GL034289