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

Citation
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
Citations number
29
Categorie Soggetti
Earth Sciences
Journal title
REMOTE SENSING OF ENVIRONMENT
ISSN journal
00344257 → ACNP
Volume
77
Issue
1
Year of publication
2001
Pages
112 - 121
Database
ISI
SICI code
0034-4257(200107)77:1<112:UOTAFT>2.0.ZU;2-N
Abstract
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.