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过去四十年来,植被绿化与土壤湿度之间的双向依存关系发生了变化。

Shifts bidirectional dependency between vegetation greening and soil moisture over the past four decades in China.

机构信息

Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China.

Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China.

出版信息

Sci Total Environ. 2023 Nov 1;897:166388. doi: 10.1016/j.scitotenv.2023.166388. Epub 2023 Aug 18.

Abstract

Soil moisture (SM) has changed significantly over the past 40 years in China, while NDVI has varied dramatically, leading to increasing regional conflict between vegetation growth and water resource use. Quantifying the bidirectional dependency between SM and NDVI is essential for understanding the balance between land vegetation and water resources. However, few studies have reported their mutual feedback and spatiotemporal bidirectional dependency. This paper aims to reveal the bidirectional dependency between SM and NDVI using Granger causality test to show spatiotemporal tendency coupling patterns through trend coupling analysis, wavelet transform, and lag correlation. The Results indicated that a coupling relationship existed between SM and NDVI over most of China. The unidirectional Granger effect between SM on NDVI was 58 %, the unidirectional Granger effect of NDVI on SM was 26 %, and the bidirectional Granger relationship between SM and NDVI was 16 %. The Granger relationship is different for different soil layers or land cover types. SM and NDVI increased together in 36 % of the land cover areas, but SM increased and NDVI decreased in 12 %, and the SM decreased and NDVI increased in 27 %. The trend coupling between SM and NDVI has spatial heterogeneity. There is no change rule of coupling relationship with drought variation, but SM and NDVI increased together with more overlapping ecological restoration projects. SM decreased with the increase of NDVI from 1982 to 2010 but has reversed since 2011. NDVI and SM co-increased significantly with the implementation of ecological restoration projects during 2011-2022. The coupling relationship has a time lag effect of 1-3 months, and the time lag of NDVI to SM of deep soil layers mainly occurred in Southern China. This study illustrated the coupling framework and feedback analysis between SM and vegetation greening, which is helpful for the scientific implementing ecological restoration projects and the management of ecosystem carbon and water cycles.

摘要

过去 40 年来,中国的土壤湿度(SM)发生了显著变化,而 NDVI 则发生了巨大变化,导致植被生长和水资源利用之间的区域冲突加剧。量化 SM 和 NDVI 之间的双向依赖关系对于理解陆地植被和水资源之间的平衡至关重要。然而,很少有研究报告它们之间的相互反馈和时空双向依赖关系。本文旨在使用格兰杰因果检验来揭示 SM 和 NDVI 之间的双向依赖关系,通过趋势耦合分析、小波变换和滞后相关来展示时空趋势耦合模式。结果表明,中国大部分地区的 SM 和 NDVI 之间存在耦合关系。SM 对 NDVI 的单向格兰杰效应为 58%,NDVI 对 SM 的单向格兰杰效应为 26%,SM 和 NDVI 之间的双向格兰杰关系为 16%。格兰杰关系因不同的土壤层或土地覆盖类型而异。在 36%的土地覆盖区域,SM 和 NDVI 一起增加,但在 12%的区域,SM 增加而 NDVI 减少,在 27%的区域,SM 减少而 NDVI 增加。SM 和 NDVI 之间的趋势耦合具有空间异质性。耦合关系没有随干旱变化的变化规律,但随着更多生态修复项目的实施,SM 和 NDVI 一起增加。从 1982 年到 2010 年,SM 随着 NDVI 的增加而减少,但自 2011 年以来已经逆转。2011-2022 年期间,随着生态修复项目的实施,NDVI 和 SM 显著协同增加。耦合关系具有 1-3 个月的时滞效应,深层土壤层中 NDVI 对 SM 的时滞主要发生在中国南方。本研究说明了 SM 和植被绿化之间的耦合框架和反馈分析,有助于科学实施生态修复项目和管理生态系统碳和水循环。

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