On the role of Rossby wave breaking in quasi‐biennial odulation of the stratospheric polar vortex

Lu, Hua ORCID:; Hitchman, Matthew H; Gray, Lesley J; Osprey, Scott M. 2020 On the role of Rossby wave breaking in quasi‐biennial odulation of the stratospheric polar vortex. Quarterly Journal of the Royal Meteorological Society, 146 (729). 1939-1959.

Before downloading, please read NORA policies.
Lu_et_al-2020-Quarterly_Journal_of_the_Royal_Meteorological_Society.pdf - Accepted Version

Download (35MB) | Preview


The boreal‐winter stratospheric polar vortex is more disturbed when the quasi‐biennial oscillation (QBO) in the lower stratosphere is in its easterly phase (eQBO), and more stable during the westerly phase (wQBO). This so‐called “Holton‐Tan effect” (HTE) is known to involve Rossby waves (RWs) but the details remain obscure. This tropical‐extratropical connection is re‐examined in an attempt to explain its intra‐seasonal variation and its relation to Rossby wave breaking (RWB). Reanalyses in isentropic coordinates from the National Center for Environmental Prediction Climate Forecast System for the 1979 – 2017 period are used to evaluate the relevant features of RWB in the context of waveguide, wave mean‐flow interaction, and the QBO‐induced meridional circulation. During eQBO, the net extratropical wave forcing is enhanced in early winter with ~25% increase in upward propagating PRWs of zonal wavenumber 1 (wave‐1). RWB is also enhanced in the lower stratosphere, characterized by convergent anomalies in the subtropics and at high‐latitudes and strengthened waveguide in between at 20‐40°N, 350‐650 K. In late winter, RWB leads to finite amplitude growth, which hinders upward propagating PRWs of zonal wavenumber 2 and 3 (wave‐2‐3). During wQBO, RWB in association with wave‐2‐3 is enhanced in the upper stratosphere. Wave absorption/mixing in the surf zone reinforces a stable polar vortex in early to middle winter. A poleward confinement of extratropical waveguide in the upper stratosphere forces RWB to extend downward around January. A strengthening of upward propagating wave‐2‐3 follows and the polar‐vortex response switches from reinforcement to disturbance around February, thus a sign reversal of the HTE in late winter.

Item Type: Publication - Article
Digital Object Identifier (DOI):
ISSN: 0035-9009
Additional Keywords: quasi-biennial oscillation, stratospheric polar vortex, Rossby wave breaking, Holton-Tan effect
Date made live: 03 Mar 2020 17:10 +0 (UTC)

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...