On the linearity of the stratospheric and Euro-Atlantic sector response to ENSO

The dependence of the winter stratospheric and Euro-Atlantic climate response on ENSO amplitude is investigated using the HadGEM3 model. Experiments are performed with imposed east Pacific sea surface temperature perturbations corresponding to Niño-3.4 anomalies of 60.75, 1.5, 2.25, and 3.0 K. In th...

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Bibliographic Details
Main Authors: Trascasa-Castro, P, Maycock, AC, Yiu, YYS, Fletcher, JK
Format: Article in Journal/Newspaper
Language:English
Published: American Meteorological Society 2019
Subjects:
Arctic
Pacific
aleutian low
North Atlantic
North Atlantic oscillation
Online Access:https://eprints.whiterose.ac.uk/147474/
https://eprints.whiterose.ac.uk/147474/8/jcli-d-18-0746_1.pdf
Description
Summary:The dependence of the winter stratospheric and Euro-Atlantic climate response on ENSO amplitude is investigated using the HadGEM3 model. Experiments are performed with imposed east Pacific sea surface temperature perturbations corresponding to Niño-3.4 anomalies of 60.75, 1.5, 2.25, and 3.0 K. In the North Pacific, El Niño (EN) deepens and shifts the Aleutian low eastward, while the equivalent magnitude La Niña (LN) perturbations drive anomalies of opposite sign that are around 4 times weaker. The muted North Pacific response to LN can be traced back to the weaker response of tropical convection and the associated anomalous Rossby wave source. The EN perturbations weaken the Arctic polar vortex, with the winter mean zonal mean zonal wind at 608N and 10 hPa decreasing approximately linearly with Niño-3.4 anomaly by around 23.6 m s21 K21 . For the strongest EN case (13 K), the frequency of sudden stratospheric warmings (SSWs) increases by ;60% compared to the control experiment. Hence the results do not support a saturation of the stratospheric pathway for strong EN as suggested in previous literature. The equivalent amplitude LN perturbations cause a weak strengthening of the polar vortex and no substantial change in SSW frequency, in contrast to some reanalysis-based studies. EN induces a negative North Atlantic Oscillation (NAO) index throughout boreal winter, which increases approximately linearly with the Niño-3.4 anomaly by around 20.6 standard deviations K21 . Only the response to the strongest LN perturbations projects onto a weak positive NAO in November, suggesting that the mechanism for the Euro-Atlantic response to LN may be distinct from EN.

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