Spatiotemporal evolution of agricultural drought and its attribution under different climate zones and vegetation types in the Yellow River Basin of China

IF 8 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Yujie Ding, Lifeng Zhang, Yi He, Shengpeng Cao, Xiao Wei, Yan Guo, Ling Ran, Mikalai Filonchyk
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Abstract

Ecological protection and high-quality development of the Yellow River Basin (YRB) are major national strategies in China. Agricultural drought (AD) is one of the most important stress factors of the ecological security of the YRB. Currently, there is a lack of exploration of the spatiotemporal evolution of AD in the YRB under different climatic zones and vegetation types, and the mechanisms by the driving factors influence AD remain unclear. The Temperature Vegetation Dryness Index (TVDI) for the YRB in China during 2000–2020 was calculated using Land Surface Temperature (LST) and the Normalized Difference Vegetation Index (NDVI). We analyzed the spatiotemporal evolution of AD from the perspective of upstream of the YRB (UYRB), midstream of the YRB (MYRB), and downstream of the YRB (DYRB), as well as different climate zones and vegetation types. The driving factors were selected based on the Pearson correlation analysis, Geographical detector, and Mantel test. Structural equation modeling (SEM) was employed to quantify the direct and indirect effects of the driving factors on AD in the YRB. We found a slowing trend of AD in the YRB, mainly in the Loess Plateau, which is distributed in UYRB and MYRB, but an increasing trend for AD in DYRB. Temperature, which is the most direct influential factor, has exacerbated AD in UYRB and MYRB. However, surface solar radiation (SSR) has the greatest constraining effect on DYRB. AD increased in arid and desert zones, while a decreasing trend is observed for other climatic zones and vegetation types. In arid and semiarid zones, human activities and SSR were the largest indirect factors exacerbating AD. In humid and subhumid zones, the largest indirect factor exacerbating AD was potential evapotranspiration (PET). Temperature is the most direct factor exacerbating AD in cropland and forest, while PET is the largest indirect factor exacerbating AD in grassland. This study elucidates the driving factors and mechanisms of AD in the YRB to provide scientific decision support for mitigating regional drought and promoting regional sustainable development.

Abstract Image

中国黄河流域不同气候带和植被类型下农业干旱的时空演变及其归因
黄河流域生态保护和高质量发展是中国的重大国家战略。农业干旱(AD)是影响黄河流域生态安全的重要胁迫因素之一。目前,对黄河流域不同气候带和植被类型下农业干旱的时空演变缺乏探索,农业干旱的驱动因素影响机制尚不清楚。本文利用地表温度(LST)和归一化植被指数(NDVI)计算了2000-2020年中国长三角地区的温度植被干燥指数(TVDI)。从长江上游、中游、下游以及不同气候带和植被类型的角度分析了 AD 的时空演变。根据皮尔逊相关分析、地理检测器和曼特尔检验选择了驱动因素。我们采用结构方程模型(SEM)来量化驱动因素对长江下游 AD 的直接和间接影响。我们发现长三角地区的 AD 有减缓的趋势,主要分布在黄土高原,黄土高原分布在 UYRB 和 MYRB 中,但在 DYRB 中 AD 有增加的趋势。温度是最直接的影响因素,它加剧了 UYRB 和 MYRB 的 AD。然而,地表太阳辐射(SSR)对干旱地区的制约作用最大。在干旱和荒漠区,AD 有所增加,而在其他气候区和植被类型中,AD 呈下降趋势。在干旱和半干旱地区,人类活动和 SSR 是加剧 AD 的最大间接因素。在湿润和亚湿润地区,加剧旱地退化的最大间接因素是潜在蒸散量(PET)。温度是加剧耕地和森林旱地退化的最直接因素,而潜在蒸散量则是加剧草地旱地退化的最大间接因素。这项研究阐明了长三角地区旱地退化的驱动因素和机制,为缓解区域干旱和促进区域可持续发展提供了科学的决策支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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