气候变化和土地利用变化对长江黄河源区生态系统净初级生产力的影响

Zhe Yuan , Qingqing Jiang , Jun Yin
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引用次数: 1

摘要

净生态系统生产力(NEP)是陆地生态系统吸收碳能力的重要指标。为了制定适应和缓解战略,必须调查气候变化和人为活动对国家环境政策的影响。本研究利用遥感图像、气候变量数据和土地利用数据分析了长江和黄河源区NEP的时空特征。然后研究了气候变化如何影响碳汇和碳源,以及土地利用的变化如何影响碳储存。根据研究结果,从2001年到2019年,SRYY每年贡献35.26 Tg C的碳汇(1 Tg=1012 g)。受气候、土壤和植被的影响,NEP在空间上表现出区域差异。NEP的空间分布从西北向东南逐渐增加。近二十年来,SRYY的NEP以每十年3.24 Tg C的速度略有上升。NEP呈上升趋势,占整个研究区的78.9%,分布广泛,在西部地区尤其显著,如沱沱河流域。NEP与气候变量的相关性分析表明,温度是SRYY中NEP的主要控制因素。在整个SRYY中,约54.4%的NEP方差是由温度引起的。然而,NEP与年降水量之间没有显著的线性关系。近二十年来,建成区土地扩张和生态退化分别使碳汇减少了28.61 Gg C(1 Gg=109 g)和1.94 Tg C。鼠患和放牧导致的草原退化是一些地区碳汇减少的主要因素。植被和湿地区域的恢复导致碳汇增加0.75 Tg C。这可能得益于气候变暖和生态保护措施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Impact of climate change and land use change on ecosystem net primary productivity in the Yangtze River and Yellow River Source Region, China

Net ecosystem productivity (NEP) is an important indicator of the capacity of terrestrial ecosystems to absorb carbon. For the purpose of developing adaptation and mitigation strategies, it is essential to investigate the effect of climatic changes and anthropogenic activities on NEP. This study analyzed the spatiotemporal properties of NEP in the Yangtze River and Yellow River Source Region (SRYY) using remote sensing images, climate variable data, and land use data. Then it was examined at how climatic change affected carbon sinks and sources and how changes in land use affected carbon storage. According to the results, the SRYY contributed a carbon sink worth 35.26 Tg C annually from 2001 to 2019 (1 Tg = 1012 g). Influenced by climate, soil and vegetation, NEP displayed regional differences in space. The spatial distribution of NEP gradually increased from Northwest to Southeast. In recent twenty years, the NEP of SRYY slightly increased with a rate of 3.24 Tg C per decade. The NEP with an increasing trend accounted for 78.9% of the whole study area, which were widely distributed and especially significant in the west, such as Tuotuo River Basin. The correlation analysis between NEP and climate variables suggested that temperature was the dominant control of NEP in the SRYY. About 54.4% of the NEP variance across the entire SRYY was contributed by temperature. However, there was no significant linear relationship between NEP and annual precipitation. In recent two decades, built-up land expansion and ecological degradation reduced carbon sink by 28.61 Gg C (1 Gg = 109 g) and 1.94 Tg C, respectively. Grassland degradation caused by rodent infestation and grazing was the main factor of carbon sink reduction in some areas. The restoration of vegetation and wetland areas resulted in a 0.75 Tg C increase in the carbon sink. It might be benefited from warmer climate condition and ecological protection measures.

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