By Wing-Huen Ip, Jai-Ho Oh, Gyan Prakash Singh
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Extra info for Advances in Geosciences: Volume 10: Atmospheric Science (As)
3(a) thick solid line), as the monsoon rainfall moves into the northern SCS with maximum in the region of 10◦ N– 15◦ N. In the northern SCS (north to 10◦ N), the decrease of humidity in ABL is coincident with a maximum rainfall moving from the southern SCS (Figs. 3(a) and (e), thick solid line). (2) A decrease of SST occurs from early to late May in the southern SCS is concurrent with a rapid increase of SST in the northern SCS April 10, 2009 12:4 AOGS 2007 - AS Volume 9in x 6in Satellite-Observed 3D Moisture Structure b672-V10-ch04 33 Fig.
A) The advance, (b) the retreat (the number in the pictures refer to the time (pentad)). April 10, 2009 12:4 AOGS 2007 - AS Volume 9in x 6in EASM and the Rainfall in East China b672-V10-ch05 45 of EASM, we divided the process of EASM’s movement into the following ﬁve phases: 1. The EASM’s onset and its front concentrates in South China On average, the Asian summer monsoon breaks out in SCS at 28th pentad. During the 28th and 29th pentad, the front stays at South China Sea (SCS) and nearby Philippine and moves northward and eastward continually.
E. Im = Q−Q Vsw − Vsw , + δsw δq (1) where Vsw is the projection of total wind speed on the SW direction at a 850 hPa for a grid point, Q is the mean speciﬁc humidity at 925 and 850 hPa for a grid point; Vsw is the projection of 850-hPa total wind speed on the SW direction, averaged over (10◦ N–50◦ N, 90◦ E–150◦E); Q is the mean speciﬁc humidity at 925 and 850 hPa over the same area; δsw and δq are the standard deviation of Vsw and Q in the above region. 3) line south (north) of 35◦ N is denoted as its leading edge.
Advances in Geosciences: Volume 10: Atmospheric Science (As) by Wing-Huen Ip, Jai-Ho Oh, Gyan Prakash Singh