The sizes of the tropical cyclones (TCs) occurring over the western North P
acific (WNP) and the North Atlantic between 1991 and 1996 are estimated to
establish a database for the study of the climatology of TC size and the ph
ysical processes responsible for the size changes of TCs. Wind data from th
e scatterometer onboard the European Remote-Sensing Satellites 1 and 2 (ERS
-1 and ERS-2) form the date source for defining the TC size. The size of a
TC is defined as the mean radius at which the relative vorticity decreases
to 1 x 10(-5) s(-1). The mean TC size is found to be 3.7 degrees lat for WN
P TCs and 3.0 degrees lat for those in the North Atlantic. Such a differenc
e in size between the two basins is statistically significant at the 95% co
nfidence level. The mean TC size in the WNP is also found to vary seasonall
y, with a value larger in the late season (October and November) than in mi
dsummer (July and August). These results generally agree with those from pr
evious studies using other measures of size. The size changes (increasing o
r decreasing) of some TCs are also identified. The high-resolution surface
wind data from the ERS satellites are shown to be a valuable tool in the st
udy of TC sizes.