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[气候变化对长江中下游地区植被总初级生产力生长季影响的定量评估]

[Quantitative Assessment of the Impact of Climate Change on the Growing Season of Vegetation Gross Primary Productivity in the Middle and Lower Reaches of the Yangtze River].

作者信息

Xu Yong, Pan Yu-Chun, Zou Bin, Zheng Zhi-Wei, Guo Zhen-Dong

机构信息

College of Geomatics and Geoinformation, Guilin University of Technology, Guilin 541006, China.

School of Geosciences and Info-physics, Central South University, Changsha 410083, China.

出版信息

Huan Jing Ke Xue. 2024 Mar 8;45(3):1615-1628. doi: 10.13227/j.hjkx.202304152.

Abstract

Quantitatively determining the direct, indirect, and comprehensive effects of climatic factors on the growing season of the vegetation GPP (GPP) in the middle and lower reaches of the Yangtze River at the regional and vegetation type scales can provide a scientific basis for the management and restoration of regional vegetation resources under the background of global climate change. Using MODIS GPP data, meteorological data, and vegetation type data, combined with Theil-Sen Median trend analysis and the Mann-Kendall significance test, the spatiotemporal characteristics of the GPP in the middle and lower reaches of the Yangtze River were investigated at different temporal and spatial scales. Path analysis was used to further reveal the direct, indirect, and comprehensive effects of climate factors on GPP variation in different vegetation types. The results showed that:① from 2000 to 2021, the vegetation GPP in the middle and lower reaches of the Yangtze River showed a fluctuating upward trend, with a rising rate (in terms of C, same below) of 2.70 g·(m·a) (<0.01). The GPP of different vegetation types all showed a significant upward trend (<0.01), with shrubs having the highest upward rate of 3.31 g·(m·a) and cultivated vegetation having the lowest upward rate of 2.54 g·(m·a). ② The proportion of the area with an upward trend in GPP in the middle and lower reaches of the Yangtze River was 88.11%. The proportion of the area with an upward trend in GPP was greater than 84% for all different vegetation types, with shrubs (49.76%) and cultivated vegetation (44.36%) having significantly higher proportions of the area with an upward trend than that in other vegetation types. ③ The path analysis results showed that precipitation and the maximum temperature had a significant positive direct effect on vegetation GPP (<0.05), whereas solar radiation had a non-significant positive effect ( ≥ 0.05). The indirect effects of maximum temperature, precipitation, and solar radiation on vegetation GPPGS were all non-significantly negative ( ≥ 0.05). Under the combined effects of direct and indirect influences, precipitation and maximum temperature had a non-significant positive effect on vegetation GPP ( ≥ 0.05), whereas solar radiation had a non-significant negative effect on vegetation GPP ( ≥ 0.05). Among different vegetation types, precipitation was the main climate factor affecting the changes in GPP of cultivated vegetation, whereas the maximum temperature was the main climate factor affecting the changes in GPP of coniferous forests, broad-leaved forests, shrubs, and grasslands. ④ The changes in vegetation GPP in the middle and lower reaches of the Yangtze River were mainly influenced by the direct effects of maximum temperature, precipitation, and solar radiation, with the direct effect of precipitation dominating 56.72% of the changes in GPP. The research results can provide a reference for quantifying the carbon sequestration potential of vegetation in the middle and lower reaches of the Yangtze River and formulating ecological restoration governance policies tailored to local conditions under the background of global climate change.

摘要

定量确定气候因子在区域和植被类型尺度上对长江中下游地区植被总初级生产力(GPP)生长季的直接、间接和综合影响,可为全球气候变化背景下区域植被资源的管理与恢复提供科学依据。利用MODIS GPP数据、气象数据和植被类型数据,结合泰尔 - 森中位数趋势分析和曼 - 肯德尔显著性检验,在不同时空尺度上研究了长江中下游地区GPP的时空特征。采用路径分析进一步揭示气候因子对不同植被类型GPP变化的直接、间接和综合影响。结果表明:①2000—2021年,长江中下游地区植被GPP呈波动上升趋势,上升速率(以碳计,下同)为2.70 g·(m²·a)⁻¹(P<0.01)。不同植被类型的GPP均呈显著上升趋势(P<0.01),其中灌木上升速率最高,为3.31 g·(m²·a)⁻¹,耕地植被上升速率最低,为2.54 g·(m²·a)⁻¹。②长江中下游地区GPP呈上升趋势的面积比例为88.11%。所有不同植被类型中GPP呈上升趋势的面积比例均大于84%,其中灌木(49.76%)和耕地植被(44.36%)呈上升趋势的面积比例显著高于其他植被类型。③路径分析结果表明,降水和最高气温对植被GPP有显著的正直接效应(P<0.05),而太阳辐射有不显著的正效应(P≥0.05)。最高气温、降水和太阳辐射对植被GPP的间接效应均为不显著的负效应(P≥0.05)。在直接和间接影响的共同作用下,降水和最高气温对植被GPP有不显著的正效应(P≥0.05),而太阳辐射对植被GPP有不显著的负效应(P≥0.05)。在不同植被类型中,降水是影响耕地植被GPP变化的主要气候因子,而最高气温是影响针叶林、阔叶林、灌木和草地GPP变化的主要气候因子。④长江中下游地区植被GPP变化主要受最高气温、降水和太阳辐射的直接效应影响,其中降水的直接效应占GPP变化的56.72%。研究结果可为量化长江中下游地区植被碳汇潜力及在全球气候变化背景下制定因地制宜的生态恢复治理政策提供参考。

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