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a
b
c
d
Fig. 27.2
Horizontal distribution of accumulated total precipitation from 1200 UTC 30 to
1200 UTC 31 August 2002 (in mm). (
a
) observation, (
b
) NOCP (
c
)KFEXand(
d
) OPTM with
a horizontal resolution of 25 km
level pressure, or maximum surface wind speed between the observations and model
solutions).
Our results indicate that such phenomena can be forecasted more accurately, at
least for heavy rainfall, via optimal parameter estimation of operational numerical
weather prediction models.
Acknowledgements
This research is supported by the Ministry of Education, Science and
Technology, Korea, through the National Research Foundation grant (No. 2009-0093464).
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