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首页> 外文期刊>Hydrology and Earth System Sciences >Precipitation ensembles conforming to natural variations derived from a regional climate model using a new bias correction scheme
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Precipitation ensembles conforming to natural variations derived from a regional climate model using a new bias correction scheme

机译:使用新的偏差校正方案,降水合奏符合从区域气候模型得出的自然变化

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摘要

This study presents a novel bias correction scheme for regional climate model (RCM) precipitation ensembles. A primary advantage of using model ensembles for climate change impact studies is that the uncertainties associated with the systematic error can be quantified through the ensemble spread. Currently, however, most of the conventional bias correction methods adjust all the ensemble members to one reference observation. As a result, the ensemble spread is degraded during bias correction. Since the observation is only one case of many possible realizations due to the climate natural variability, a successful bias correction scheme should preserve the ensemble spread within the bounds of its natural variability (i.e. sampling uncertainty). To demonstrate a new bias correction scheme conforming to RCM precipitation ensembles, an application to the Thorverton catchment in the south-west of England is presented. For the ensemble, 11 members from the Hadley Centre Regional Climate Model (HadRM3-PPE) data are used and monthly bias correction has been done for the baseline time period from 1961 to 1990. In the typical conventional method, monthly mean precipitation of each of the ensemble members is nearly identical to the observation, i.e. the ensemble spread is removed. In contrast, the proposed method corrects the bias while maintaining the ensemble spread within the natural variability of the observations.
机译:这项研究为区域气候模型(RCM)降水集合提出了一种新颖的偏差校正方案。使用模型集成进行气候变化影响研究的主要优势在于,可以通过集合传播来量化与系统误差相关的不确定性。然而,当前,大多数常规偏差校正方法将所有合奏成员调整为一个参考观察。结果,在偏差校正期间整体扩展变差。由于由于气候自然变异性,观测只是许多可能实现的一种情况,因此成功的偏差校正方案应将系谱散布保持在其自然变异性(即采样不确定性)的范围内。为了证明符合RCM降水集合的新的偏差校正方案,提出了在英格兰西南部的Thorverton流域的应用。对于合奏,使用了Hadley中心区域气候模型(HadRM3-PPE)数据的11个成员,并已对1961年至1990年的基准时间段进行了月度偏差校正。在典型的常规方法中,每个月平均降水量集合成员与观察值几乎相同,即去除了集合传播。相反,所提出的方法在保持观测值自然变化范围内的整体扩展的同时校正了偏差。

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