Abstract

Abstract This paper is an examination of 2–3-day convective variability in the tropical Pacific region. The initial focus of the paper is on the western tropical Pacific during the Tropical Ocean Global Atmosphere Coupled Ocean-Atmosphere Response Experiment (TOGA COARE) intensive observation period (IOP); high spatial and temporal resolution outgoing longwave radiation (OLR) data and sea surface temperatures are filtered to eliminate diurnal and lower-frequency variability. The propagation of the 2–3-day convective variability is also studied. Westward propagation appears to be favored in some regions, indicative of the events being influenced by westward-propagating inertio-gravity waves. However, many regions have 2–3-day events that divide fairly equally into eastward and westward propagations, indicating that both eastward- and westward-propagating inertio-gravity waves are influencing the oscillation. The SST data during the 4-month IOP dataset show evidence of a 2–3-day variability during those con...

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