用局部回归和分位数映射相结合的方法模拟环流模型偏差

Benjamin Washington, L. Seymour, T. Mote
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引用次数: 0

摘要

摘要总环流模型(GCM)的输出是气候变化影响评估的主要信息来源。然而,GCM原始数据很少直接用于区域规模的影响评估,因为它们经常包含系统性错误或偏差。在这篇文章中,我们提出了一种对标准分位数映射的新扩展,该扩展允许使用局部回归来实现偏差幅度的连续季节性变化。我们的主要目标是在波多黎各热带地区进行更大规模的统计缩减工作的背景下检查该工具的有效性,在那里,本地化缩减可能特别具有挑战性。在此过程中,我们利用多元填充算法来估计横跨波多黎各的不完全气候数据网络中的缺失数据。接下来,我们应用多变量缩减方法的组合,从两种碳排放情景下的三个环流模型(RCP4.5和RCP8.5)中生成波多黎各23个地点的现场气候预测。最后,我们的偏差校正方法被应用于这些缩小规模的GCM气候预测。这些偏差校正方法允许GCM偏差作为用户定义季节(此处为儒略日)的函数而变化。使用连续曲线而不是移动窗口或每月中断来估计偏移。选定乐团的结果一致认为,波多黎各将在下个世纪继续变暖。在RCP4.5强迫情景下,我们的方法表明旱季的降雨量将增加,而早雨季和晚雨季的总降雨量可能会下降。我们应用于RCP8.5强迫情景的方法有利于波多黎各的湿润气候,这是由于波多黎各雨季早期(4月至7月)和雨季后期(8月至11月)高强度降雨事件的频率增加所致。
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Modeling general circulation model bias via a combination of localized regression and quantile mapping methods
Abstract. General circulation model (GCM) outputs are a primary source of information for climate change impact assessments. However, raw GCM data rarely are used directly for regional-scale impact assessments as they frequently contain systematic error or bias. In this article, we propose a novel extension to standard quantile mapping that allows for a continuous seasonal change in bias magnitude using localized regression. Our primary goal is to examine the efficacy of this tool in the context of larger statistical downscaling efforts on the tropical island of Puerto Rico, where localized downscaling can be particularly challenging. Along the way, we utilize a multivariate infilling algorithm to estimate missing data within an incomplete climate data network spanning Puerto Rico. Next, we apply a combination of multivariate downscaling methods to generate in situ climate projections at 23 locations across Puerto Rico from three general circulation models in two carbon emission scenarios: RCP4.5 and RCP8.5. Finally, our bias-correction methods are applied to these downscaled GCM climate projections. These bias-correction methods allow GCM bias to vary as a function of a user-defined season (here, Julian day). Bias is estimated using a continuous curve rather than a moving window or monthly breaks. Results from the selected ensemble agree that Puerto Rico will continue to warm through the coming century. Under the RCP4.5 forcing scenario, our methods indicate that the dry season will have increased rainfall, while the early and late rainfall seasons will likely have a decline in total rainfall. Our methods applied to the RCP8.5 forcing scenario favor a wetter climate for Puerto Rico, driven by an increase in the frequency of high-magnitude rainfall events during Puerto Rico's early rainfall season (April to July) as well as its late rainfall season (August to November).
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来源期刊
Advances in Statistical Climatology, Meteorology and Oceanography
Advances in Statistical Climatology, Meteorology and Oceanography Earth and Planetary Sciences-Atmospheric Science
CiteScore
4.80
自引率
0.00%
发文量
9
审稿时长
26 weeks
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