Abstract
The nonstationarity of the intraseasonal oscillations (ISOs) associated with the western North Pacific summer monsoon (WNPSM) is examined using a wavelet analysis of outgoing longwave radiation (OLR). Both the 10-20- and 30-60-day ISOs are found to display significant interannual modulations, and their relative strengths vary with time. The variation of OLR associated with a strong ISO, either 10-20- or 30-60-day, could be as large as 20 W m-2 in magnitude. Case studies showed that the mechanism for development of low OLR may differ in individual years, and that the 10-20-day ISO, the 30-60-day ISO, and the seasonal cycle may each become dominant in different years. © 2006 American Meteorological Society.
| Original language | English |
|---|---|
| Pages (from-to) | 622-629 |
| Journal | Journal of Climate |
| Volume | 19 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 15 Feb 2006 |
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