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200 - Typhoon Committee

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ESCAP/WMO<br />

<strong>Typhoon</strong> <strong>Committee</strong> Annual Review <strong>200</strong>7<br />

c. Interaction with Users, Other Members<br />

and/or Other Components<br />

There are no updates this year.<br />

d. Training Progress<br />

d.1 Seventh <strong>Typhoon</strong> <strong>Committee</strong> training seminar<br />

JMA, which is in charge of the Regional Specialized<br />

Meteorological Centre for tropical cyclones within the<br />

framework of the WMO (through the RSMC Tokyo -<br />

<strong>Typhoon</strong> Center), assists <strong>Typhoon</strong> <strong>Committee</strong> (TYC)<br />

Members in the improvement of typhoon monitoring<br />

through the provision of typhoon analysis/forecast<br />

products and the implementation of typhoon analysis/<br />

forecast training.<br />

As part of these activities, the Center has conducted<br />

an annual TYC Training Seminar at JMA headquarters<br />

in agreement with the TYC since <strong>200</strong>1. In <strong>200</strong>7, the<br />

seventh seminar was held from 18 to 27 July with the<br />

participation of two female forecasters from Cambodia<br />

and the Philippines. In the seminar, they received onthe-job<br />

training in typhoon analysis using the SATAID<br />

software developed by JMA, and attended lectures on<br />

typhoon analysis/forecasting as well as the typhoonrelated<br />

operations of JMA.<br />

As no tropical cyclone formed for tracking during the<br />

seminar, the forecasters tackled the Dvorak analysis<br />

using previous satellite images of tropical cyclones<br />

including MAN-YI (0704).<br />

Figure 4 Seventh <strong>Typhoon</strong> <strong>Committee</strong> training seminar<br />

d.2 Group training course in meteorology<br />

JMA has conducted group training courses in<br />

meteorology since 1973, and the course was renewed<br />

in <strong>200</strong>3. The current training course focuses on the<br />

utilization of satellite data including neph-analysis, and<br />

the application of numerical weather predictions and<br />

climate information/data. In September <strong>200</strong>7, the threemonth<br />

course for the year started with eight participants<br />

from eight countries, including Thailand from among<br />

the TC member countries.<br />

d.3 Dispatch of an expert to the roving seminar<br />

In September <strong>200</strong>7, JMA dispatched an expert to the<br />

roving seminar held in Manila to lecture on the topic<br />

of The Interaction of Tropical Cyclones with Monsoon<br />

Systems.<br />

d.4 Technical cooperation<br />

Since July <strong>200</strong>6, Japan has implemented a technical<br />

cooperation project in Lao PDR with a view to developing<br />

human resources on meteorology and hydrology<br />

through the Japan International Cooperation Agency<br />

(JICA). The project is scheduled for continuation until<br />

the beginning of 2010.<br />

An expert dispatched in December <strong>200</strong>6 by JICA to the<br />

Department of Meteorology in Cambodia continues to<br />

be engaged in the rehabilitation/improvement of civil<br />

aviation meteorology in the country. The expert is<br />

scheduled to be in Cambodia until early next year.<br />

e. Research Progress<br />

e.1 Improvement of the initialization scheme for tropical<br />

cyclones<br />

JMA has confirmed an improvement in numerical<br />

tropical cyclone (TC) track prediction as a result of<br />

modifying the operational initialization scheme for TCs<br />

(i.e. the <strong>Typhoon</strong>-Bogus scheme) in the global spectral<br />

model (GSM-TL959L60).<br />

In the <strong>Typhoon</strong>-Bogus scheme, several “pseudo”<br />

observational data are deployed inside a circle around<br />

the observed center position of the TC. These data are<br />

taken into account in the 4D-VAR global data assimilation<br />

process. The radius of the circle is called the Bogus-<br />

Radius. While this value for each TC of Tropical Storm<br />

(TS) intensity or higher is specified with a function of<br />

the radius of 30 kt winds and the Coriolis parameter<br />

at the center of the TC, a fixed radius of 360 km has<br />

been used as the Bogus-Radius for tropical depressions<br />

(TDs), since TDs have no analysis of the 30 kt wind<br />

radius.<br />

However, the fixed Bogus-Radius for TDs has occasionally<br />

worked inadequately and failed in appropriately<br />

correcting erroneous TD positions in the first-guess<br />

field. To alleviate the problem, a function has been<br />

introduced to enable variation of the Bogus-Radius<br />

for TDs depending on their strength and latitudinal<br />

location. The newly introduced Bogus-Radius for TDs<br />

is defined as a function of their central pressure and<br />

the latitude of their center position, with a lower limit<br />

36

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