Authors: Jianyun Gao Tim Li
Publish Date: 2012/10/19
Volume: 29, Issue: 6, Pages: 1279-1291
Abstract
The interannual variability of occurrence of multiple tropical cyclone MTC events during June–October in the western North Pacific WNP was examined for the period 1979–2006 The number of the MTC events ranged from 2 to 9 per year exhibiting a remarkable yeartoyear variation Seven active and seven inactive MTC years were identified Compared to the inactive years tropical cyclone genesis locations extended farther to the east and in the meridional direction during the active MTC years A composite analysis shows that inactive MTC years were often associated with the El Niño decaying phase as warm SST anomalies in the equatorial easterncentral Pacific in the preceding winter transitioned into cold sea surface temperature SST anomalies in the concurrent summer Associated with the SST evolution were suppressed lowlevel cyclonic vorticity and weakened convection in the WNP monsoon regionIn addition to the mean flow difference significant differences between active and inactive MTC years were also found in the strength of the atmospheric intraseasonal oscillation ISO Compared with inactive MTC years ISO activity was much stronger along the equator and in the WNP region during active MTC years Both westward and northwardpropagating ISO spectrums strengthened during active MTC years compared to inactive years The combined mean state and ISO activity changes may set up a favorable environment for the generation of MTC events
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