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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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161<br />

seasons sometimes brought great damages in the Taiwan area. On the other h<strong>and</strong>,<br />

rainfall is also a very important water resource to the isl<strong>and</strong>. A raingauge network<br />

consisting of 74 surface weather stations <strong>and</strong> 126 self- recording raingauges was<br />

set up by Central Weather Bureau in the past few years. Five conventional radars<br />

constitute the radar network(Fig.l). Two S-b<strong>and</strong> radars have provided digital<br />

data since 1985 summer. The other three radars have also provided digital data<br />

since 1988. The first Doppler radar was set up in 1987 by CAA(Civil Aeronautics<br />

Administration) at CKS( Chiang Kai-Shek) airport(Fig.2) in Taiwan area. This<br />

radar has proved its ability to observe precipitaiton systems in northern Taiwan.<br />

A field program of the Taiwan Area Mesoscale Experiment (TAMEX) was<br />

operated from 1 May to 29 June, 1987 in the Taiwan area. Three Doppler radars<br />

were positioned along the west coast of Taiwan, forming a triple Doppler network<br />

(Fig.2). The primary scientific objective of TAMEX is to improve our underst<strong>and</strong>ing<br />

of the mesoscale dynamics of the convective systems responsible for heavy precipitation.<br />

In May <strong>and</strong> June 1986, a field experiment called " TAMEX phase I"<br />

was held in Taiwan area as a testing field program for 1987 TAMEX.<br />

The mesoscale data sets of two cases in TAMEX phase I, 1986 <strong>and</strong> TAMEX<br />

,1987 were analyzed to study the characteristics of convective system during Mei-<br />

Yu season. Based on the digital radar data, a detailed discussion of the reflectivity<br />

characteristics such as horizontal pattern, vertical structure <strong>and</strong> movement was<br />

illustrated. In order to underst<strong>and</strong> the kinematics of the convective systems in<br />

TAMEX phase I, the internal motion fields of thise case were also calculated<br />

through the TREC technique. In the TAMEX case study, structural features <strong>and</strong><br />

internal motion of one long-lived <strong>and</strong> slow moving MCS rainb<strong>and</strong> originated from<br />

the Mei-Yu frontal unstable zone which occurred on 25 June 1987 in IOP-13 over<br />

the Taiwan area were investigated .<br />

2. RADAR ESTIMATE <strong>AND</strong> GUAGE MEASUREMENT<br />

During the TAMEX phase I period, digital radar data with 0.5-hr interval <strong>and</strong><br />

rain gauge data with 10 minutes interval in the major events are available. From<br />

May 20 to May 21 1986,a precipitation system was observed across the Taiwan<br />

Strait. It later brought a rainfall accumulation of approxmately 200 mm in two<br />

days in some major cities in the central <strong>and</strong> northern Taiwan. From 2300 May<br />

20 to 0700 May 21, sixteen reflectivity distributions for every 30 minutes were

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