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Rainfall was observed onboard the research vessel Mirai on 21 days during the observation period of 25 days.
The heaviest rainfall was observed in Tochigi prefecture where more than 650mm (25in) was recorded in a 24-hour period, well over twice the average monthly total for September.
In August, cool weather (average temperature of 2 3 °C below the norm) with a deficit of rainfall was observed.
The daily maximum rainfall was observed around 2300 LT on average, about 4 h later than at Bengkulu on the western coast of Sumatra Island.
Rainfall was observed to rise rapidly reaching a peak period in late May while vegetation response (NDVI) reached a peak period in early August.
Furthermore, within a specific county characterized by great systematic spatial variations of rainfall and topography across the landscape, a significant (P < 0.01) and positive linear relationship (r2 = 0.81) between local 137Cs inventory and corresponding local annual rainfall was observed.
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The maximum rainfall is observed in the monsoon months.
The d-excess values in rainfall are observed to be above ten with an average of 14.2.
Belowground at the MIU, gravity decreases that reflected mass increases above the gravimeter due to rainfall were observed.
Increased rainfall is observed in the works of Kannan and Ghosh (2011) and Rupa Kumar et al. (2006).
The result further shows that a noticeable decline in rainfall is observed from 1997 to 1998 in Kuyu district.
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