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arXiv 2401.08697physics.ao-ph

地表蒸散在区域气候模拟中的作用:评估与近期未来变化

The role of the surface evapotranspiration in regional climate modelling: Evaluation and near-term future changes

Matilde García-Valdecasas Ojeda, Juan José Rosa-Cánovas, Emilio Romero-Jiménez, P. Yeste, Sonia R. Gámiz-Fortis, Yolanda Castro-Díez, María Jesús Esteban-Parra

AI总结:

本研究利用WRF区域气候模型,结合ERA-Interim再分析资料和CMIP5全球气候模型驱动数据,评估了伊比利亚半岛地表蒸散的时空格局,并预估其在2021-2050年近期未来将显著减少,尤其在南部和夏季,揭示了地表蒸散在区域陆地-大气过程中的关键调节作用。

摘要:

地表蒸散(SFCEVP)在气候中起着至关重要的作用,是水文循环和能量循环之间的纽带。因此,如何对其进行近似处理及其在区域气候中的影响,是理解气候变化效应的重要方面,尤其是在伊比利亚半岛(IP)等过渡带地区。本研究旨在利用区域气候模型(RCM)——天气研究与预报(WRF)模型,研究SFCEVP的时空格局。为此,使用不同的驱动数据完成了一组WRF模拟。首先,开展了由ERA-Interim再分析资料驱动的近期现在(1980-2017年)模拟,以评估该RCM性能的适用性。另一方面,使用来自CMIP5计划的两个全球气候模型(GCM),即CCSM4和MPI-ESM-LR,作为驱动数据来评估GCM-RCM耦合,这对气候变化应用至关重要。最后,还研究了近期未来(2021-2050年)范式下的预估变化。总体而言,结果表明WRF模型是研究IP地区SFCEVP时空格局的有价值工具,在不同时空尺度上表现出总体可接受的能力。关于预估,结果表明IP地区在不久的将来SFCEVP可能发生显著变化。这些变化在最南部地区将更为明显,尤其是在春季和夏季,其中夏季SFCEVP将从根本上减少。这些结果与土壤湿度的预估变化一致,而土壤湿度的变化可能与降水格局的变化有关。此外,结果揭示了SFCEVP在调节该区域气候中的主要作用,这涉及复杂的陆地-大气过程。

英文摘要:

The surface evapotranspiration (SFCEVP) plays an essential role in climate, being the link between the hydrological and energy cycles. Therefore, how it is approximated and its implication in the regional climate are important aspects to understand the effects of climate change, especially over transitional zones such as the Iberian Peninsula (IP). This study aims to investigate the spatiotemporal patterns of the SFCEVP using a regional climate model (RCM), the Weather Research and Forecasting (WRF) model. With this purpose, a set of WRF simulations were completed using different driving data. On the first hand, a recent present (1980-2017) simulation driven by the ERA-Interim reanalysis was carried out to evaluate the suitability of the RCM performance. On the other hand, two global climate models (GCMs) from the CMIP5 initiative, the CCSM4 and the MPI-ESM-LR, were used as driving data to evaluate the GCM-RCM couplings, which is essential to climate change applications. Finally, projected changes were also investigated for a near-term future (2021-2050) paradigm. In general, the results pointed out the WRF model as a valuable tool to study the spatiotemporal patterns of the SFCEVP in the IP, showing an overall and acceptable ability at different spatial and temporal scales. Concerning projections, the results indicate that the IP is likely to undergo significant changes in the SFCEVP in the near future. These changes will be more apparent over the southernmost, and particularly during spring and summer, being in the latter season the SFCEVP fundamentally reduced. These results agree with projected changes in soil moisture, which is probably associated with changes in precipitation patterns. Additionally, the results reveal the major role of SFCEVP in modulating the climate over this region, which is involved in the complex land-atmosphere processes.

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