Ak. Varma et al., Use of TOPEX altimeter for the study of diurnal and spatial distribution of southwest monsoon rainfall over the Bay of Bengal and the Arabian Sea, REMOT SEN E, 77(1), 2001, pp. 112-121
In this paper, the rain detection capability of the dual-frequency (Ku and
C band) radar altimeter onboard, the non-sun-synchronous TOPEX/Poseidon (T/
P) satellite is exploited to study the diurnal variability of rainfall over
Indian oceanic regions during the southwest monsoon season. The study is d
one using three consecutive years (1993, 1994 and 1995) of T/P altimeter da
ta. Based on the difference of normalized backscattered coefficient, Delta
sigma degrees (C-Ku band), the T/P satellite observations are categorized i
nto three different classes of "no rain." "low rain," and "high rain." The
data is further divided into 12 time intervals of 2 h each, starting from 0
000 to 2400 Z. The uneven distribution of observations in each time interva
l due to orbit characteristics of T/P satellite is removed. The histograms
of rain events are plotted for the Bay of Bengal and the Arabian Sea to stu
dy diurnal and regional variability of rain events. The variation of rainfa
ll intensity, within "high-rain" category, over the two regions is also stu
died. The results showed that there is no consistent diurnal variability of
rainfall exist over the Arabian Sea and the Bay of Bengal regions from yea
r to year. However, the 3-year composite data shows more rain events over t
he Arabian Sea at early morning hours between 0000 and 0200 GMT. This is ve
rified by concurrently available TOPEX Microwave Radiometer (TMR) observati
ons of rain events. The intensity of rain rate also does not show any marke
d diurnal variability. The probability of rain events is significantly high
over the Bay of Bengal region compared to the Arabian Sea region. This is
also verified with TMR-based analysis. Further, interannual variability of
rain events and amount over the two regions from Delta sigma degrees -based
analysis is also discussed in association with interannual variations in t
he monsoon activities over these two regions. (C) 2001 Elsevier Science Inc
. All rights reserved.