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Dynamical Downscaling Simulation and Future Projection of Extreme Precipitation Activities in Taiwan during the Mei-Yu Seasons

机译:梅雨期台湾极端降水活动的动态降尺度模拟及未来预测

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?By using the Weather Research and Forecasting (denoted as WRF) model driven by two super-high-resolution global models, High Resolution Atmospheric Model (denoted as HiRAM) and Meteorological Research Institute Atmospheric General Circulation Model (denoted as MRI), this study investigates the dynamical downscaling simulation and projection of extreme precipitation activities (including intensity and frequency) in Taiwan during the Mei-Yu seasons (May and June). The analyses focus on two time period simulations: the present-day (1979-2003, historical run) and the future (2075-2099, RCP8.5 scenario). For the present-day simulation, our results show that the bias of HiRAM and MRI in simulating the extreme precipitation activities over Taiwan can be reduced after dynamical downscaling by using the WRF model. For the future projections, both the dynamical downscaling models (i.e., HiRAM-WRF and MRI-WRF) project that extreme precipitation will become more frequent and more intense over western Taiwan but less frequent and less intense over eastern Taiwan. The east-west contrast in the projected changes in extreme precipitation in Taiwan are found to be a local response to the enhancement of southwesterly monsoonal flow over the coastal regions of South China, which leads to an increase in water vapor convergence over the windward side (i.e., western Taiwan) and a decrease in water vapor convergence over the leeward side (i.e., eastern Taiwan). Further examinations of the significance of the projected changes in extreme precipitation that affect the agriculture regions of Taiwan show that the southwestern agriculture regions will be affected by extreme precipitation events more frequently and more intensely than the other subregions. This finding highlights the importance of examining regional differences in the projected changes in extreme precipitation over the complex terrain of East Asia.
机译:通过使用由两个超高分辨率全球模型,高分辨率大气模型(表示为HiRAM)和气象研究所大气总环流模型(表示为MRI)驱动的天气研究和预报(表示为WRF)模型,本研究研究了梅雨季节(5月和6月)台湾极端降水活动(包括强度和频率)的动态降尺度模拟和预测。分析着重于两个时间段模拟:今天(1979-2003,历史运行)和未来(2075-2099,RCP8.5情景)。对于当前的模拟,我们的结果表明,使用WRF模型在动态缩小比例之后,可以降低HiRAM和MRI在模拟台湾极端降水活动中的偏差。对于未来的预测,两个动态降尺度模型(即HiRAM-WRF和MRI-WRF)都预测极端降水在台湾西部将变得更加频繁和密集,而在台湾东部则将变得不那么频繁且强度较小。发现台湾地区极端降水的预计变化中的东西向差异是对华南沿海地区西南季风流动增强的局部反应,这导致向上风侧的水汽会聚增加(即台湾西部)和背风面(台湾东部)水汽汇聚减少。对影响台湾农业地区的极端降水预计变化的意义的进一步研究表明,西南农业地区将比其他分区更频繁,更强烈地受到极端降水事件的影响。这一发现强调了研究东亚复杂地形上极端降水预计变化中区域差异的重要性。

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