T. Fujii, STATISTICAL-ANALYSIS OF THE CHARACTERISTICS OF SEVERE TYPHOONS HITTING THE JAPANESE MAIN ISLANDS, Monthly weather review, 126(4), 1998, pp. 1091-1097
Characteristics of 51 severe typhoons hitting the Japanese main island
s with central pressure equal to or less than 980 hPa during the perio
d 1955-94 were analyzed by an objective method using hourly station ob
servation during typhoon passages. Position of a typhoon center, centr
al pressure depth Delta p, and radius of the maximum wind r(m), were o
btained at hourly intervals after landfall on the main islands of Japa
n. The pressure profile of severe typhoons used in this analysis was c
hosen from formulas presented in previous papers, namely the same as o
ne used by the U.S. Army Corps of Engineers for hurricanes hitting Flo
rida. Coastlines of the main islands were divided into three sections:
areas A, B, and C extending from west to east. Statistical analyses o
f parameters were made for each area. At time of landfall, the maximum
value of Delta p was 83.2 hPa for area A, 85.2 hPa for area B, and 47
.8 hPa for area C. The differences in return period of Delta p among a
reas are considered to be caused by the SST distribution off the Pacif
ic coast. On average, typhoons making landfall in area C have larger r
(m) and speed, and display a more eastward component of translation th
an those in the other two areas. The differences of speed and directio
n among areas and months can be explained to be caused by variation of
the synoptic-scale air current at the 500-hPa level.