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The stochastic typhoon event set contains 33,012 events in 1000 years of repetition.
In practice, typhoon-induced quasi-static responses measured from the field mix with temperature-induced responses because temperature varies significantly during a typhoon event.
The annual maximum wave height and the concomitant water level have been obtained by simulating the annual extreme typhoon event for 50 consecutive years.
We compared forest structure and regeneration patterns between undisturbed and disturbed stands 30 years after a typhoon event in the treeline ecotone of the Changbai Mountains, Northeastern China.
During this typhoon event, most MR amplitude enhancements appeared to correspond to the lower atmospheric disturbance area associated with the typhoon.
They then used rainfall, sediment discharge, and flow discharge data from another typhoon event to validate this threshold as a predictor of landslides and resultant sediment discharge.
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The influences of typhoon events and typhoon profiles were considered in the wind climate study.
Accurate rainfall-runoff modeling during typhoon events is an essential task for natural disaster reduction.
We selected the typhoon events used in our analyses as follows.
Validation results pertaining to three typhoon events further demonstrate that the adjustment models can reduce radar rainfall errors.
Hourly rainfall data observed at 126 raingauges in typhoon events provide the ground-truth information for adjusting radar rainfall estimates.
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