[Impact of Climate Change and Human Activities on Net Primary Productivity of Vegetation in the Yunnan-Guizhou Plateau].

Q2 Environmental Science
Yi-Fei Zhang, Jun-Ling Zhang
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Abstract

Vegetation net primary productivity (NPP) is a key indicator for assessing the carbon budget of terrestrial ecosystems. Studying the impact of climate change and human activities on vegetation NPP is critical for a deeper understanding of carbon cycling mechanisms and promoting sustainable economic development. Based on MOD17A3 NPP data, meteorological data, and land use data, this study explores the spatiotemporal variation characteristics of NPP across different geological backgrounds and vegetation types in the Yunnan-Guizhou Plateau from 2001 to 2020, using the Theil-Sen Median slope estimator and Mann-Kendall significance test. An improved residual analysis method is employed to investigate the relative contributions of climate change and human activities to vegetation NPP in the Yunnan-Guizhou Plateau. The results indicated the following: From 2001 to 2020, the NPP of vegetation in the Yunnan-Guizhou Plateau showed an increasing trend at a rate of 3.39 g·(m2·a)-1. The multi-year average NPP of vegetation in non-karst areas was 901.42 g·(m2·a)-1, which was higher than the 837.83 g·(m2·a)-1 in karst areas. However, the growth rate of vegetation NPP in non-karst areas was 2.56 g·(m2·a)-1, which was lower than the 3.69 g·(m2·a)-1 in karst areas. Among different types of vegetation, herbaceous vegetation had the highest multi-year average NPP at 900.26 g·(m2·a)-1, with a relatively high growth rate of 3.6 g·(m2·a)-1. Arbor vegetation had a higher multi-year average NPP of 864.54 g·(m2·a)-1 but the lowest growth rate at only 2.69 g·(m2·a)-1. Economic vegetation had a lower multi-year average NPP of 809.24 g·(m2·a)-1 but a higher growth rate of 3.96 g·(m2·a)-1. Precipitation contributed positively to vegetation NPP in the Yunnan-Guizhou Plateau, with a positive contribution rate of 68.16%, while temperature had a positive contribution rate of 74.5%. Precipitation significantly promoted vegetation growth in the central and eastern regions of the Yunnan-Guizhou Plateau but had a suppressive effect on vegetation in the western regions. From 2001 to 2020, climate change contributed 77.09% to the changes in vegetation NPP in the Yunnan-Guizhou Plateau, which was higher than the 22.91% contribution from human activities. Human activities had a positive contribution rate of 70.76% to vegetation NPP in karst areas, higher than the 60.96% in non-karst areas. Human activities had a larger positive contribution rate to herbaceous vegetation NPP at 73.02% and to shrub vegetation at 71.92%. The findings provide a theoretical basis for formulating tailored ecological restoration and management strategies for the Yunnan-Guizhou Plateau.

气候变化和人类活动对云贵高原植被净初级生产力的影响[j]。
植被净初级生产力(NPP)是评估陆地生态系统碳收支的重要指标。研究气候变化和人类活动对植被NPP的影响,对于深入认识碳循环机制和促进经济可持续发展具有重要意义。基于MOD17A3 NPP数据、气象数据和土地利用数据,利用Theil-Sen Median slope estimator和Mann-Kendall显著性检验,探讨了2001 - 2020年云黔高原不同地质背景和植被类型下NPP的时空变化特征。采用改进的残差分析方法,研究了气候变化和人类活动对云贵高原植被NPP的相对贡献。结果表明:2001 ~ 2020年,云贵高原植被NPP以3.39 g·(m2·a)-1的速率呈增加趋势;非喀斯特地区植被多年平均NPP为901.42 g·(m2·a)-1,高于喀斯特地区的837.83 g·(m2·a)-1。非喀斯特地区植被NPP的增长率为2.56 g·(m2·a)-1,低于喀斯特地区的3.69 g·(m2·a)-1。不同类型植被中,草本植被的多年平均NPP最高,为900.26 g·(m2·a)-1,增长率较高,为3.6 g·(m2·a)-1。乔木植被多年平均NPP较高,为864.54 g·(m2·a)-1,但生长率最低,仅为2.69 g·(m2·a)-1。经济植被多年平均NPP较低,为809.24 g·(m2·a)-1,但生长率较高,为3.96 g·(m2·a)-1。降水对云贵高原植被NPP的正贡献为68.16%,而温度对植被NPP的正贡献为74.5%。在云贵高原中部和东部地区,降水对植被生长有显著的促进作用,而对西部地区则有抑制作用。2001 - 2020年,气候变化对云贵高原植被NPP变化的贡献率为77.09%,高于人类活动对植被NPP变化的贡献率(22.91%)。人类活动对喀斯特地区植被NPP的正贡献率为70.76%,高于非喀斯特地区的60.96%。人类活动对草本植被NPP和灌木植被NPP的正贡献率较大,分别为73.02%和71.92%。研究结果为制定有针对性的云贵高原生态恢复与管理策略提供了理论依据。
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
环境科学
环境科学 Environmental Science-Environmental Science (all)
CiteScore
4.40
自引率
0.00%
发文量
15329
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