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Sensitivity of the Latitude of the Westerly Jet Stream to Climate Forcing

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2019GL086563· OSTI ID:1599466
 [1];  [1];  [2]
  1. Department of Atmospheric and Oceanic Sciences University of California Los Angeles CA USA
  2. Atmospheric Sciences and Global Change Division Pacific Northwest National Laboratory Richland WA USA
Abstract

The latitude of the westerly jet stream is influenced by a variety of climate forcings, but their effects on the jet latitude often manifest as a tug of war between tropical forcing (e.g., tropical upper‐tropospheric warming) and polar forcing (e.g., Antarctic stratospheric cooling or Arctic amplification). Here we present a unified forcing‐feedback framework relating different climate forcings to their forced jet changes, in which the interactions between the westerly jet and synoptic eddies are synthesized by a zonal advection feedback, analogous to the feedback framework for assessing climate sensitivity. This framework is supported by a prototype feedback analysis in the atmospheric dynamical core of a climate model with diverse thermal and mechanical forcings. Our analysis indicates that the latitude of a westerly jet is most sensitive to the climate change‐induced jet speed changes near the tropopause. The equatorward jet shift also displays a larger deviation from linearity than the poleward counterpart.

Sponsoring Organization:
USDOE
OSTI ID:
1599466
Alternate ID(s):
OSTI ID: 1605422
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 4 Vol. 47; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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