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East Asia and Western Pacific METEOROLOGY AND CLIMATE

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449<br />

THE OPERATIONAL GLOBAL FORECAST SYSTEM AT CENTRAL WEATHER BUREAU<br />

Chuen-Teyr Terng<br />

Computer Center, Central Weather Bureau,<br />

Taipei, China<br />

ABSTRACT<br />

Because of the limitations of subjective weather forecasting <strong>and</strong><br />

the advantages of numerical weather forecasting (NWP), the Central<br />

Weather Bureau (CWB) has begun a five-year project to establish a NWP<br />

system. Due to the fact that Taiwan is situated at the boundary of a<br />

large continent (the Euro-<strong>Asia</strong> continent) <strong>and</strong> a large ocean (the<br />

<strong>Pacific</strong>), <strong>and</strong> also the fact that Taiwan is located in the sub-tropical<br />

region, being affected by different weather systems in winter <strong>and</strong> in<br />

summer, four different NWP models are required. The four models are :<br />

Global (for 5 to 7-day forecast <strong>and</strong> 4-D data assimilation), Regional<br />

(for 2-day forecast <strong>and</strong> weather patterns of the <strong>Asia</strong>n area), Mesoscale<br />

(for 1 day forecast <strong>and</strong> weather patterns around Taiwan), <strong>and</strong> Typhoon<br />

Track (tracking typhoon movements around Taiwan). Besides these<br />

models, there is a control system, which automatically monitors the<br />

entire system, <strong>and</strong> a data-acquisition system.<br />

A super computer (CDC-205) <strong>and</strong> a computer for the front end (CDC-<br />

840) were installed in CWB in December 1986. Beginning in July 1987,<br />

the global model underwent testing <strong>and</strong> it was declarea operational in<br />

July 1988. The global model composes of three parts : analysis,<br />

initialization <strong>and</strong> forecasting. The objective analysis portion uses<br />

FIB <strong>and</strong> Barnes's schemes for the analyses of sea-level surface<br />

pressure <strong>and</strong> upper air mass <strong>and</strong> wind field.. The initialization scheme<br />

uses variational method. The UCLA general circulation model forms the<br />

basis of the forecasting part.<br />

The procedure of the global model is as follows : The global<br />

observations are transmitted to CWB through GWDI <strong>and</strong> JWA's satellite<br />

network. The data are then decoded <strong>and</strong> error-checked by CWB's frontend<br />

computer. The data are then transmitted to the super-computer for<br />

sea-level surface pressure analysis, upper air mass field <strong>and</strong> wind<br />

field analyses, <strong>and</strong> initialization, all on isobaric coordinates. The<br />

data are next interpolated to sigma-coordinates. Forecasting<br />

computations are performed as the next step. The forecast results are<br />

interpolated back to isobaric coordinates <strong>and</strong> drawn as weather charts<br />

for use by the forecasters.<br />

With the advancement of numerical methods, the enlargement of<br />

computer memory <strong>and</strong> the arrival of faster computers, NWP is facing<br />

rapid improvements. In view of this, CWB is planning its 2nd<br />

generation of NWP system. This includes the introduction of optimal<br />

initialization, normal model initializationj spectral forecasting<br />

model <strong>and</strong> more advanced physical parameterization. We hope that in the<br />

near future, our forecasting capabilities can be compared with those<br />

of the most advanced operational centers of the world.

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