英文摘要 |
The most uncertainty for precipitation observation is the limitation of definitely picturing out spatial distribution characteristics of the actual rainfall. From past debris flow events, the l rain-gauge stations are the major source to provide rainfall information on the warnings of debris flow. Through the interpolation of rain-gauge data by Kriging, IDW, or Barnes methods, we are able to get a rough estimation and understanding on precipitation. The interpolated precipitation forecast from rain-gauge figures is often incapable of reflecting the actual condition and will sometimes yield a questionable measurement. This research adopts the radar detection, updated every 10 minutes, from the QPESUMS system provided by the Central Weather Bureau for analyzing rainfall characteristics and integrating this data with the surface rain-gauge observations. The 1.3 km X 1.3 km grid of the radar data is much finer than rain gauge observation. Furthermore, radar can estimate moisture content in the air; it can be used as a reference for surface rainfall estimates. Rain gauges only report the pinpoint data at very limited location. Therefore, estimations of surface rainfall distribution are obtained by a series of interpolation methods. From extensive case study results, the Kriging method is more effective than Barnes. Therefore, it can be used in the future for precipitation standards during instant disaster warnings to improve the uncertainty of the errors in the current rainfall estimation. |