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A Statistical-Based Model for Typhoon Rain Hazard Assessment

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Extreme typhoon rainfall can lead to damaging floods near the coastal region in mainland China. In the present study, we calibrate the parameters for a parametric hurricane rain model by using the precipitation radar (PR) data from the Tropical Rainfall Measuring Mission (TRMM) (i.e., PR-TRMM) and the TRMM microwave imager (TMI) data (i.e., TMI-TRMM). To show the applicability of the model for the tropical cyclone (TC) rain hazard assessment, we combine the developed rainfall intensity model with historical and synthetic TC tracks to estimate the T-year return period value of the accumulated rainfall in 24 h, QA24-T. We map QA24-100 for part of the coastal region in mainland China, showing that the spatial variation of QA24-100 is relatively smooth. It was found that the estimated QA24-100 using the model developed, based on the snapshots from PR-TRMM, is about 60% of that obtained using the model developed based on the snapshots from TMI-TRMM. This reflects the differences in the rainfall intensities reported in TMI-TRMM and PR-TRMM. As part of verification, we compare the estimated return period value to that obtained by using the record from surface meteorological stations at a few locations. The comparison indicates that, on average, QA24-100 based on gauge data is about 1.4 and 2.3 times that obtained using the model developed based on the snapshots from PR-TRMM and TRM-TRMM, respectively. This suggests that, for TC rain hazard estimation, one may consider the empirical scaling factor of 1.4 and 2.4 for the rainfall intensity models developed based on snapshots from PR-TRMM and TMI-TRMM, respectively.
Title: A Statistical-Based Model for Typhoon Rain Hazard Assessment
Description:
Extreme typhoon rainfall can lead to damaging floods near the coastal region in mainland China.
In the present study, we calibrate the parameters for a parametric hurricane rain model by using the precipitation radar (PR) data from the Tropical Rainfall Measuring Mission (TRMM) (i.
e.
, PR-TRMM) and the TRMM microwave imager (TMI) data (i.
e.
, TMI-TRMM).
To show the applicability of the model for the tropical cyclone (TC) rain hazard assessment, we combine the developed rainfall intensity model with historical and synthetic TC tracks to estimate the T-year return period value of the accumulated rainfall in 24 h, QA24-T.
We map QA24-100 for part of the coastal region in mainland China, showing that the spatial variation of QA24-100 is relatively smooth.
It was found that the estimated QA24-100 using the model developed, based on the snapshots from PR-TRMM, is about 60% of that obtained using the model developed based on the snapshots from TMI-TRMM.
This reflects the differences in the rainfall intensities reported in TMI-TRMM and PR-TRMM.
As part of verification, we compare the estimated return period value to that obtained by using the record from surface meteorological stations at a few locations.
The comparison indicates that, on average, QA24-100 based on gauge data is about 1.
4 and 2.
3 times that obtained using the model developed based on the snapshots from PR-TRMM and TRM-TRMM, respectively.
This suggests that, for TC rain hazard estimation, one may consider the empirical scaling factor of 1.
4 and 2.
4 for the rainfall intensity models developed based on snapshots from PR-TRMM and TMI-TRMM, respectively.

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