| 摘要(英) |
In this study, several statistical tests including Mann-Whitney-Pettitt, Kruskal-Wallis variance analysis and Mann-Kendall trend test were employed to examine whether significant shifts and trends of hydrological and meteorological data can be identified with long-term observational records from 1971 to 2010. This is helpful to understand characteristics of regional hydrological and meteorological variations. Using seasonal outlooks provided by the Central Weather Bureau (CWB), a weather generator was used to generate multimembers of daily weather data to drive the hydrological model to estimate future inflows. Then a system dynamic model was employed to compute projected reservoir storages and available water supplies. The Deficit Percent Day (DPD) Index is further employed to assess variations of carrying capacity of the the Dahan River water supply system.
Results of statistical analyses indicate the shift of most hydro-meteorological observations occurred around 1977 to 1983. It is therefore concluded that there are significant variations in hydrometeorology of the Shihmen reservoir watershed for the past 30 years.
Regarding the trends, the increasing trends in yearly precipitation, wet season precipitation, typhoon season precipitation, the number of rainy days with 0 to 0.49 mm/day, the number of rainy days with 81 to 200 mm/day, and most station precipitation were found. On the other hand, the decreasing trends in number of rainy days with 0.5 to 10 mm/day, air temperature of 10-year and 20-year time series, pan evaporation were found. The increasing trend of yearly precipitation is strongly correlated with the increase of precipitation during typhoon seasons. Besides, the number of rainy days for both 0 to 0.49 mm/day and 81 to 200 mm/day were found increase indicating changes of rainfall patterns toward unproductive rains and torrential rains.
Precipitation projected with the CWB climate forecasts are all greater than observations and the temperature forecasts are underestimated in the study case of 2015. The estimates of inflows and reservoir stages are both higher than observed values as higher projected rainfall. The lead-1 water level simulations with the statistical-downscaling climate forecasts released in February are close to observed values, which is caused by higher inflow will lead to higher discharge and is not the real match of projections.
The DPDs of the Dahan River water supply system were given with three grades determined by two thresholds of exceedance probabilities of 0.3 and 0.7 by using historical inflows as indices of drought risks. Combining different reservoir initial stages and all possible projected rainfalls in February, March, and April, drought risks of each combination can be evaluated in advance. When reservoir stage is below 225m, it is suggested to implement restricted management measures no matter what kind of projected rainfalls. When the projected rainfall of February is normal, there is high possibility of the DPD greater than 1000 in conjunction with reservoir stages below 230m. When the projected rainfall of February is below normal, there is high risk of water shortage. Under the conditions of having below normal rainfall projections for two months, the case occurred in February and March will lead to higher risk of drought than the case occurred in February and April, and less risk for the case of March and April. With graded DPD indices, it can help better decision making for water resources agency during drought. |
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