N. Hirasawa et al., ABRUPT CHANGE IN THE CHARACTERISTICS OF THE CLOUD ZONE IN SUBTROPICALEAST-ASIA AROUND THE MIDDLE OF MAY, Journal of the Meteorological Society of Japan, 73(2), 1995, pp. 221-239
An abrupt seasonal change in cloud features around the East Asian clou
d band (EA-band) was found in the middle of May or late May in all the
years of 1982 to 1987 by using two indexes derived from GMS infrared
data, middle- and high-level cloud amount (MHc-amount) and the appeara
nce frequency of the high-level cloud region (Hc-frequency) for a 10-
or 15-day period. The change occurred over a short period, less than 5
days (transition period: TP), nearly simultaneously with the onset of
the ''Southeast Asian summer monsoon'' about one month before the ons
et of the Indian monsoon. The main results are as follows: 1) The MHc-
amount and Hc-frequency increase considerably in the coastal region of
South China after the TP. The greater part of the Hc-frequency are as
sociated with the deep convective clouds. This change is associated wi
th the enhancement of the low-level southwesterly wind, an decrease in
thickness of baroclinic layer below the 500 mb level and an increase
in specific humidity there and in the region to the south of the EA-ba
nd. 2) MHc-amount and Hc-frequency in the EA-band also increase to the
east of 130 degrees E after the TP, accompanied by the enhancement of
the southwesterly wind in its southern part and the southward shift o
f a subtropical high pressure area west of 150 degrees E. 3) As for th
e year-to-year variation, the distribution of the area with large MHc-
amount in the EA-band before the TP seems to be greatly influenced by
the amount of confluence between the southwesterly wind in the north o
f the subtropical high pressure area and westerly wind north of the EA
-band. 4) MHc-amount over Central China after the TP is about 60 % in
the year of stronger baroclinicity there, but is about 20 % in the yea
r of weaker baroclinicity. 5) Only in 1987, the EA-band and a subtropi
cal high pressure area east of 130 degrees E shifted northward after t
he TP, which are the opposite characteristics to all the other years.