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The global response to tropical heating in the Madden–Julian oscillation during the northern winter
Author(s) -
Matthews Adrian J.,
Hoskins Brian J.,
Masutani Michiko
Publication year - 2004
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1256/qj.02.123
Subject(s) - extratropical cyclone , madden–julian oscillation , climatology , rossby wave , convection , geology , equatorial waves , longitude , zonal flow (plasma) , environmental science , forcing (mathematics) , atmospheric sciences , equator , latitude , meteorology , geography , physics , plasma , geodesy , quantum mechanics , tokamak
A life cycle of the Madden–Julian oscillation (MJO) was constructed, based on 21 years of outgoing long‐wave radiation data. Regression maps of NCEP–NCAR reanalysis data for the northern winter show statistically significant upper‐tropospheric equatorial wave patterns linked to the tropical convection anomalies, and extratropical wave patterns over the North Pacific, North America, the Atlantic, the Southern Ocean and South America. To assess the cause of the circulation anomalies, a global primitive‐equation model was initialized with the observed three‐dimensional (3D) winter climatological mean flow and forced with a time‐dependent heat source derived from the observed MJO anomalies. A model MJO cycle was constructed from the global response to the heating, and both the tropical and extratropical circulation anomalies generally matched the observations well. The equatorial wave patterns are established in a few days, while it takes approximately two weeks for the extratropical patterns to appear. The model response is robust and insensitive to realistic changes in damping and basic state. The model tropical anomalies are consistent with a forced equatorial Rossby–Kelvin wave response to the tropical MJO heating, although it is shifted westward by approximately 20 ° longitude relative to observations. This may be due to a lack of damping processes (cumulus friction) in the regions of convective heating. Once this shift is accounted for, the extratropical response is consistent with theories of Rossby wave forcing and dispersion on the climatological flow, and the pattern correlation between the observed and modelled extratropical flow is up to 0.85. The observed tropical and extratropical wave patterns account for a significant fraction of the intraseasonal circulation variance, and this reproducibility as a response to tropical MJO convection has implications for global medium‐range weather prediction. Copyright © 2004 Royal Meteorological Society