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美国玉米带增强了区域降水再循环。

US Corn Belt enhances regional precipitation recycling.

作者信息

Zhang Zhe, He Cenlin, Chen Fei, Miguez-Macho Gonzalo, Liu Changhai, Rasmussen Roy

机构信息

Advanced Study Program, NSF National Center for Atmospheric Research, Boulder, CO 80301.

Research Applications Laboratory, NSF National Center for Atmospheric Research, Boulder, CO 80301.

出版信息

Proc Natl Acad Sci U S A. 2025 Jan 7;122(1):e2402656121. doi: 10.1073/pnas.2402656121. Epub 2024 Dec 30.

Abstract

Precipitation recycling, where evapotranspiration (ET) from the land surface contributes to precipitation within the same region, is a critical component of the water cycle. This process is especially important for the US Corn Belt, where extensive cropland expansions and irrigation activities have significantly transformed the landscape and affected the regional climate. Previous studies investigating precipitation recycling typically relied on analytical models with simplifying assumptions, overlooking the complex interactions between groundwater hydrology and agricultural management. In this study, we use high-resolution climate models coupled with an explicit water vapor tracer algorithm to quantify the impacts of shallow groundwater, dynamic crop growth, and irrigation on regional precipitation recycling in the US Corn Belt. We find that these coupled groundwater-crop-irrigation processes reduce surface temperatures and increase the growing season precipitation. The increase in precipitation is attributed to a significant enhancement of the precipitation recycling ratio from 14 to 18%. This enhanced precipitation recycling is stronger in a dry year than normal and wet years, depending on both large-scale moisture transport and local ET. Our study underscores the critical role of groundwater hydrology and agricultural management in altering the regional water cycle, with important implications for regional climate predictions and food and water security.

摘要

降水再循环是指陆地表面的蒸发散(ET)对同一区域内的降水有贡献,它是水循环的一个关键组成部分。这一过程对美国玉米带尤为重要,在那里,大规模的农田扩张和灌溉活动显著改变了地貌并影响了区域气候。以往研究降水再循环的研究通常依赖于带有简化假设的分析模型,忽略了地下水文与农业管理之间的复杂相互作用。在本研究中,我们使用高分辨率气候模型并结合显式水汽示踪算法,来量化浅层地下水、动态作物生长和灌溉对美国玉米带区域降水再循环的影响。我们发现,这些地下水-作物-灌溉耦合过程降低了地表温度并增加了生长季降水量。降水量的增加归因于降水再循环比率从14%显著提高到18%。这种增强的降水再循环在干旱年份比正常年份和湿润年份更强,这取决于大规模水汽输送和当地的蒸发散。我们的研究强调了地下水文和农业管理在改变区域水循环方面的关键作用,对区域气候预测以及粮食和水资源安全具有重要意义。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/ae20/11725895/99d2edeb6389/pnas.2402656121fig01.jpg

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