Comparison of CMIP6 model performance in estimating human thermal load in Europe in the winter season

IF 3.5 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES International Journal of Climatology Pub Date : 2024-06-02 DOI:10.1002/joc.8526
Zsófia Szalkai, E. Kristóf, A. Zsákai, F. Ács
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Abstract

In this work, historical simulations of CMIP6 GCMs are evaluated with respect to the ERA5 reanalysis dataset, in order to examine their ability to assess human thermal load in Europe in the winter season. The period of 1981–2010 is chosen for the analysis, and thermal load is expressed via the clothing resistance index (rcl index; expressed in clo). It is found that the GCMs are able to reproduce the areal differences of thermal load satisfactorily, the spatial correlation with the reanalysis is greater than 0.95 in all cases. The effects of the main geographical constraints (latitude, continentality and elevation) are shown by all GCM simulations, as rcl index values are greater at higher latitudes, away from the ocean and in mountainous areas, although GCMs only capture major mountains (the Caucasus, the Armenian Highlands, the Scandinavian Mountains, the Alps). The root‐mean‐square error (RMSE) is around 0.2 clo in all cases, GCMs generally perform better in homogenous lowland areas, while results are less accurate in highlands and mountains owing to the coarse horizontal resolution of GCMs (~1°). The smallest errors occur over central and western Europe and the Mediterranean region, while results tend to be less accurate over the northeastern part of Europe. Biases in the estimation of heat deficit can mainly be attributed to biases in temperature, but biases in wind speed and atmospheric downward radiation seem to be important factors as well.
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CMIP6 模型在估算欧洲冬季人体热负荷方面的性能比较
在这项工作中,针对ERA5 再分析数据集对 CMIP6 GCM 的历史模拟进行了评估,以检查其评估欧洲冬季人体热负荷的能力。分析选择了 1981-2010 年这一时期,热负荷通过衣物阻力指数(rcl 指数,以 clo 表示)来表示。研究发现,大气环流模型能够令人满意地再现热负荷的区域差异,与再分析的空间相关性在所有情况下都大于 0.95。所有 GCM 模拟都显示了主要地理限制因素(纬度、大陆性和海拔)的影响,因为 rcl 指数值在高纬度、远离海洋和多山地区更大,尽管 GCM 只捕捉到主要山脉(高加索山脉、亚美尼亚高原、斯堪的纳维亚山脉和阿尔卑斯山脉)。在所有情况下,均方根误差 (RMSE) 约为 0.2 clo,GCM 在同质低地地区的表现一般较好,而在高地和山区,由于 GCM 的水平分辨率较低(约 1°),结果的准确性较差。欧洲中部和西部以及地中海地区的误差最小,而欧洲东北部的结果往往不太准确。热量损失估计的偏差主要归因于温度偏差,但风速和大气向下辐射的偏差似乎也是重要因素。
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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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