Institute of Industrial Science, The University of Tokyo, 5-1-5, Kashiwanoha, Kashiwa-Shi, Chiba, 277-8574, Japan.
Sci Rep. 2023 Jun 9;13(1):9412. doi: 10.1038/s41598-023-36489-3.
Ensemble simulations of climate models are used to assess the impact of climate change on precipitation, and require downscaling at the local scale. Statistical downscaling methods have been used to estimate daily and monthly precipitation from observed and simulated data. Downscaling of short-term precipitation data is necessary for more accurate prediction of extreme precipitation events and related disasters at the regional level. In this study, we developed and investigated the performance of a downscaling method for climate model simulations of hourly precipitation. Our method was designed to recognize time-varying precipitation systems that can be represented at the same resolution as the numerical model. Downscaling improved the estimation of the spatial distribution of hourly precipitation frequency, monthly average, and 99th percentile values. The climate change in precipitation amount and frequency were shown in almost all areas by using the 50 ensemble averages of estimated precipitation, although the natural variability was too large to compare with observations. The changes in precipitation were consistent with simulations. Therefore, our downscaling method improved the evaluation of the climatic characteristics of extreme precipitation events and more comprehensively represented the influence of local factors, such as topography, which have been difficult to evaluate using previous methods.
集合模拟的气候模型被用于评估气候变化对降水的影响,并且需要在当地尺度上进行降尺度。统计降尺度方法已被用于从观测和模拟数据中估计日和月降水量。短期降水数据的降尺度对于在区域尺度上更准确地预测极端降水事件和相关灾害是必要的。在这项研究中,我们开发并研究了一种用于小时降水气候模型模拟的降尺度方法的性能。我们的方法旨在识别可以在与数值模型相同的分辨率下表示的时变降水系统。降尺度提高了对小时降水频率、月平均值和 99 百分位数空间分布的估计。通过使用估计降水的 50 个集合平均值,几乎在所有地区都显示了降水数量和频率的气候变化,尽管自然变异性太大,无法与观测结果进行比较。降水的变化与模拟结果一致。因此,我们的降尺度方法改进了对极端降水事件气候特征的评估,并更全面地表示了局部因素的影响,例如地形,这是以前的方法难以评估的。