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DOI | 10.5194/esd-15-167-2024 |
Impact of groundwater representation on heat events in regional climate simulations over Europe | |
Poshyvailo-Strube, Liubov; Wagner, Niklas; Goergen, Klaus; Furusho-Percot, Carina; Hartick, Carl; Kollet, Stefan | |
发表日期 | 2024 |
ISSN | 2190-4979 |
EISSN | 2190-4987 |
起始页码 | 15 |
结束页码 | 2 |
卷号 | 15期号:2 |
英文摘要 | The representation of groundwater is simplified in most regional climate models (RCMs), potentially leading to biases in the simulations. This study introduces a unique dataset from the regional Terrestrial Systems Modelling Platform (TSMP) driven by the Max Planck Institute Earth System Model at Low Resolution (MPI-ESM-LR) boundary conditions in the context of dynamical downscaling of global climate models (GCMs) for climate change studies. TSMP explicitly simulates full 3D soil and groundwater dynamics together with overland flow, including complete water and energy cycles from the bedrock to the top of the atmosphere. By comparing the statistics of heat events, i.e., a series of consecutive days with a near-surface temperature exceeding the 90th percentile of the reference period, from TSMP and those from GCM-RCM simulations with simplified groundwater dynamics from the COordinated Regional Climate Downscaling EXperiment (CORDEX) for the European domain, we aim to improve the understanding of how groundwater representation affects heat events in Europe.The analysis was carried out using RCM outputs for the summer seasons of 1976-2005 relative to the reference period of 1961-1990. While our results show that TSMP simulates heat events consistently with the CORDEX ensemble, there are some systematic differences that we attribute to the more realistic representation of groundwater in TSMP. Compared to the CORDEX ensemble, TSMP simulates fewer hot days (i.e., days with a near-surface temperature exceeding the 90th percentile of the reference period) and lower interannual variability and decadal change in the number of hot days on average over Europe. TSMP systematically simulates fewer heat waves (i.e., heat events lasting 6 d or more) compared to the CORDEX ensemble; moreover, they are shorter and less intense. The Iberian Peninsula is particularly sensitive with respect to groundwater. Therefore, incorporating an explicit 3D groundwater representation in RCMs may be a key in reducing biases in simulated duration, intensity, and frequency of heat waves in Europe. The results highlight the importance of hydrological processes for the long-term regional climate simulations and provide indications of possible potential implications for climate change projections. |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:001190498400001 |
来源期刊 | EARTH SYSTEM DYNAMICS
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/290776 |
作者单位 | Helmholtz Association; Research Center Julich; INRAE; Helmholtz Association; Research Center Julich |
推荐引用方式 GB/T 7714 | Poshyvailo-Strube, Liubov,Wagner, Niklas,Goergen, Klaus,et al. Impact of groundwater representation on heat events in regional climate simulations over Europe[J],2024,15(2). |
APA | Poshyvailo-Strube, Liubov,Wagner, Niklas,Goergen, Klaus,Furusho-Percot, Carina,Hartick, Carl,&Kollet, Stefan.(2024).Impact of groundwater representation on heat events in regional climate simulations over Europe.EARTH SYSTEM DYNAMICS,15(2). |
MLA | Poshyvailo-Strube, Liubov,et al."Impact of groundwater representation on heat events in regional climate simulations over Europe".EARTH SYSTEM DYNAMICS 15.2(2024). |
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