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泛欧地下水-大气陆地系统气候学的物理一致性模拟。

Pan-European groundwater to atmosphere terrestrial systems climatology from a physically consistent simulation.

机构信息

Agrosphere (IBG-3), Research Centre Jülich, 52428, Jülich, Germany.

Centre for High-Performance Scientific Computing in Terrestrial Systems, Geoverbund ABC/J, 52428, Jülich, Germany.

出版信息

Sci Data. 2019 Dec 16;6(1):320. doi: 10.1038/s41597-019-0328-7.

Abstract

Applying the Terrestrial Systems Modeling Platform, TSMP, this study provides the first simulated long-term (1996-2018), high-resolution (~12.5 km) terrestrial system climatology over Europe, which comprises variables from groundwater across the land surface to the top of the atmosphere (G2A). The data set offers an unprecedented opportunity to test hypotheses related to short- and long-range feedback processes in space and time between the different interacting compartments of the terrestrial system. The physical consistency of simulated states and fluxes in the terrestrial system constitutes the uniqueness of the data set: while most regional climate models (RCMs) have a tendency to simplify the soil moisture and groundwater representation, TSMP explicitly simulates a full 3D soil- and groundwater dynamics, closing the terrestrial water cycle from G2A. As anthopogenic impacts are excluded, the dataset may serve as a near-natural reference for global change simulations including human water use and climate change. The data set is available as netCDF files for the pan-European EURO-CORDEX domain.

摘要

本研究应用陆地系统建模平台(TSMP),首次提供了欧洲地区长期(1996-2018 年)、高分辨率(约 12.5km)的陆地系统气候模拟,涵盖了从陆地表面到大气层顶部的地下水等变量(G2A)。该数据集提供了一个前所未有的机会,可用于测试关于陆地系统不同相互作用部分之间的空间和时间上的短期和长期反馈过程的假设。陆地系统中模拟状态和通量的物理一致性构成了数据集的独特性:虽然大多数区域气候模式(RCM)倾向于简化土壤湿度和地下水表示,但 TSMP 明确模拟了完整的 3D 土壤和地下水动态,从 G2A 封闭陆地水循环。由于排除了人为影响,该数据集可作为包括人类用水和气候变化在内的全球变化模拟的近自然参考。该数据集以 netCDF 文件的形式提供,适用于整个欧洲的 EURO-CORDEX 区域。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/e4b4/6914794/3f380f2e11e0/41597_2019_328_Fig1_HTML.jpg

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