Why Do Similar Patterns of Tropical Convection Yield Extratropical Circulation Anomalies of Opposite Sign?

Tropical precipitation anomalies associated with El Niño and Madden–Julian oscillation (MJO) phase 1 (La Niña and MJO phase 5) are characterized by a tripole, with positive (negative) centers over the Indian Ocean and central Pacific and a negative (positive) center over the warm pool region. Howeve...

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Veröffentlicht in:	Journal of the atmospheric sciences 2017-02, Vol.74 (2), p.487-511
Hauptverfasser:	Goss, Michael, Feldstein, Steven B.
Format:	Artikel
Sprache:	eng
Schlagworte:	Anomalies Atmospheric precipitations Circulation Climate Climate models Climatology Convection Convection modes Cyclones Dynamic height El Nino El Nino phenomena Equator Geopotential Geopotential height Heating Height anomalies La Nina Madden-Julian oscillation Observational studies Oceans Precipitation Precipitation anomalies Studies Tropical climate Tropical convection Weather forecasting Yields
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