Interannual Variability of Summer Monsoon Onset over the Western North Pacific and the Underlying Processes

TLDR: In this paper, the authors studied the onset of the summer monsoon over the South China Sea (SCS) and the western North Pacific (WNP) and found that the onset anomaly exhibits an in-phase interannual variation across the entire WNP domain.

Abstract: Climatological summer monsoon onset over the South China Sea (SCS) and the western North Pacific (WNP) (defined as the region of 108‐208N, 1208‐1608E) displays three distinct stages. Around mid-May, monsoon rain commences in the SCS and the Philippines. In early to mid-June, the monsoon rain extends to the southwestern Philippine Sea. After mid-July, the rainy season starts in the northeastern part of the WNP. The onset anomaly, however, displays an in-phase interannual variation across the entire WNP domain. The standard deviation of the onset date increases eastward from 3 pentads in the SCS to 5 pentads in the northeastern part of the domain. The large onset variability in the WNP is mainly attributed to large year-to-year changes of the seasonal cycle. .