首页> 外文期刊>Hydrological Research Letters >Dynamic downscaling and bias correction of rainfall in the Pampanga River Basin, Philippines, for investigating flood risk changes due to global warming
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Dynamic downscaling and bias correction of rainfall in the Pampanga River Basin, Philippines, for investigating flood risk changes due to global warming

机译:菲律宾潘邦加河流域的降雨动态降尺度和降雨偏差校正,用于调查全球变暖导致的洪水风险变化

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The Pampanga River Basin in Philippines suffers from floods due to typhoons or monsoonal rainfall every year. Assessment of changes in flood risk due to global warming is, therefore, an important issue for this flood-vulnerable basin. We studied possible changes in rainfall features under present (1979–2003) and future (2075–2099) climates using dynamic downscaling of MRI-AGCM experiments. The GCM projections were downscaled into a finer resolution of 5 km for hydrological simulation (catchment size of 10,500 km2). The downscaled rainfall overestimated the number of weak rainfall events, which subsequently resulted in overestimation of monthly rainfall. Bias correction was carried out for downscaled rainfall with reference to raingauge rainfall to perform cumulative distribution mapping. The simulation results found that monthly rainfall would change slightly between present and future climate conditions, with extreme rainfall very likely to increase in the future. The annual maximum 48 h rainfall with a 50-year return period may increase from 320 mm under the present climate to 470 mm (MRI-AGCM 3.2S) or 530 mm (MRI-AGCM 3.2H) under the RCP8.5 future climate scenario. This increase in extreme rainfall in the future would have a significant impact on this vulnerable river basin.
机译:菲律宾的邦板牙河流域每年因台风或季风降雨而遭受洪灾。因此,对全球变暖造成的洪水风险变化进行评估,对于这个易受洪灾的盆地来说是一个重要的问题。我们使用MRI-AGCM实验的动态降尺度研究了当前(1979-2003年)和未来(2075-2099年)气候下降雨特征的可能变化。将GCM投影缩小到更精细的分辨率5 km以进行水文模拟(集水面积10,500 km 2 )。降雨减少导致高估了弱降雨事件的数量,随后导致高估了每月降雨。参照雨量计降雨对小尺度降雨进行了偏差校正,以进行累积分布图绘制。模拟结果发现,在当前和未来的气候条件下,每月降雨量将略有变化,未来极有可能增加极端降雨。 RMO8.5未来气候情景下,在50年恢复期的年最大48小时降雨量可能从当前气候下的320 mm增加到470 mm(MRI-AGCM 3.2S)或530 mm(MRI-AGCM 3.2H) 。未来极端降雨的增加将对该脆弱的流域产生重大影响。

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