The circulation response to volcanic eruptions

The key roles of stratospheric warming and eddy interactions

Kevin Dallasanta, Edwin Gerber, Matthew Toohey

Research output: Contribution to journalArticle

Abstract

Proxy data and observations suggest that large tropical volcanic eruptions induce a poleward shift of the North Atlantic jet stream in boreal winter. However, there is far from universal agreement in models on this effect and its mechanism, and the possibilities of a corresponding jet shift in the Southern Hemisphere or the summer season have received little attention. Using a hierarchy of simplified atmospheric models, this study examines the impact of stratospheric aerosol on the extratropical circulation over the annual cycle. In particular, the models allow the separation of the dominant shortwave (surface cooling) and longwave (stratospheric warming) impacts of volcanic aerosol. It is found that stratospheric warming shifts the jet poleward in both the summer and winter hemispheres. The experiments cannot definitively rule out the role of surface cooling, but they provide no evidence that it shifts the jet poleward. Further study with simplified models demonstrates that the response to stratospheric warming is remarkably generic and does not depend critically on the boundary conditions (e.g., the planetary wave forcing) or the atmospheric physics (e.g., the treatment of radiative transfer and moist processes). It does, however, fundamentally involve both zonal-mean and eddy circulation feedbacks. The time scales, seasonality, and structure of the response provide further insight into the mechanism, as well as its connection to modes of intrinsic natural variability. These findings have implications for the interpretation of comprehensive model studies and for postvolcanic prediction.

Original languageEnglish (US)
Pages (from-to)1101-1120
Number of pages20
JournalJournal of Climate
Volume32
Issue number4
DOIs
StatePublished - Feb 1 2019

Fingerprint

eddy
volcanic eruption
warming
cooling
volcanic aerosol
jet stream
planetary wave
winter
summer
annual cycle
seasonality
Southern Hemisphere
radiative transfer
boundary condition
aerosol
timescale
prediction
experiment

Keywords

  • Atmosphere
  • Empirical orthogonal functions
  • General circulation models
  • Volcanoes

ASJC Scopus subject areas

  • Atmospheric Science

Cite this

The circulation response to volcanic eruptions : The key roles of stratospheric warming and eddy interactions. / Dallasanta, Kevin; Gerber, Edwin; Toohey, Matthew.

In: Journal of Climate, Vol. 32, No. 4, 01.02.2019, p. 1101-1120.

Research output: Contribution to journalArticle

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