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首页> 外文期刊>Hydrology and Earth System Sciences >Precipitation bias correction of very high resolution regional climate models
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Precipitation bias correction of very high resolution regional climate models

机译:超高分辨率区域气候模型的降水偏差校正

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Regional climate models are prone to biases in precipitation that are problematic for use in impact models such as hydrology models. A large number of methods have already been proposed aimed at correcting various moments of the rainfall distribution. They all require that the model produce the same or a higher number of rain days than the observational data sets, which are usually gridded data sets. Models have traditionally met this condition because their spatial resolution was coarser than the observational grids. But recent climate simulations use higher resolution and the models are likely to systematically produce fewer rain days than the gridded observations. brbr In this study, model outputs from a simulation at 2 km resolution are compared with gridded and in situ observational data sets to determine whether the new scenario calls for revised methodologies. The gridded observations are found to be inadequate to correct the high-resolution model at daily timescales, because they are subjected to too frequent low intensity precipitation due to spatial averaging. A histogram equalisation bias correction method was adapted to the use of station, alleviating the problems associated with relative low-resolution observational grids. The wet-day frequency condition might not be satisfied for extremely dry biases, but the proposed approach substantially increases the applicability of bias correction to high-resolution models. The method is efficient at bias correcting both seasonal and daily characteristic of precipitation, providing more accurate information that is crucial for impact assessment studies.
机译:区域气候模型容易产生降水偏差,这在诸如水文模型的影响模型中难以使用。已经提出了许多旨在校正降雨分布的各个时刻的方法。他们都要求模型产生的降雨天数与观测数据集(通常是网格数据集)相同或更多。传统上,模型满足此条件是因为它们的空间分辨率比观察网格要粗糙。但是最近的气候模拟使用更高的分辨率,并且该模型可能比网格观测系统地产生更少的降雨天数。 在这项研究中,将2 km分辨率的模拟输出与网格和现场观测数据集进行比较,以确定新方案是否需要修订的方法。发现网格化的观测值不足以在每日时标上校正高分辨率模型,因为由于空间平均,它们经受了过于频繁的低强度降水。直方图均衡偏差校正方法适用于测站的使用,减轻了与相对低分辨率观测网格相关的问题。对于极端干燥的偏差,可能无法满足湿天频率条件,但是所提出的方法大大提高了偏差校正对高分辨率模型的适用性。该方法可有效地校正降水的季节性和每日特征,从而提供更准确的信息,这对于影响评估研究至关重要。

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