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气候因素对长江源区净初级生产力的影响。

Effects of climatic factors on the net primary productivity in the source region of Yangtze River, China.

机构信息

Changjiang River Scientific Research Institute, Changjiang Water Resources Commission of the Ministry of Water Resources of China, Wuhan, China.

Hubei Key Laboratory of Water Resources & Eco-Environmental Sciences, Wuhan, 430010, China.

出版信息

Sci Rep. 2021 Jan 14;11(1):1376. doi: 10.1038/s41598-020-80494-9.

Abstract

The ecosystem of the Source Region of Yangtze River (SRYR) is highly susceptible to climate change. In this study, the spatial-temporal variation of NPP from 2000 to 2014 was analyzed, using outputs of Carnegie-Ames-Stanford Approach model. Then the correlation characteristics of NPP and climatic factors were evaluated. The results indicate that: (1) The average NPP in the SRYR is 100.0 gC/m from 2000 to 2014, and it shows an increasing trend from northwest to southeast. The responses of NPP to altitude varied among the regions with the altitude below 3500 m, between 3500 to 4500 m and above 4500 m, which could be attributed to the altitude associated variations of climatic factors and vegetation types; (2) The total NPP of SRYR increased by 0.18 TgC per year in the context of the warmer and wetter climate during 2000-2014. The NPP was significantly and positively correlated with annual temperature and precipitation at interannual time scales. Temperature in February, March, May and September make greater contribution to NPP than that in other months. And precipitation in July played a more crucial role in influencing NPP than that in other months; (3) Climatic factors caused the NPP to increase in most of the SRYR. Impacts of human activities were concentrated mainly in downstream region and is the primary reason for declines in NPP.

摘要

长江源区生态系统对气候变化高度敏感。本研究利用卡内基-梅隆-斯坦福方法模型的输出,分析了 2000 年至 2014 年 NPP 的时空变化,并评估了 NPP 与气候因子的相关特征。结果表明:(1)2000 年至 2014 年,长江源区平均 NPP 为 100.0gC/m,呈现出从西北向东南逐渐增加的趋势。NPP 对海拔的响应因地区而异,在海拔低于 3500m、3500m 至 4500m 之间以及高于 4500m 的地区,这归因于与海拔相关的气候因子和植被类型的变化;(2)在 2000-2014 年温暖湿润的气候条件下,长江源区的总 NPP 每年增加 0.18TgC。NPP 与年气温和年降水在年际时间尺度上呈显著正相关。2 月、3 月、5 月和 9 月的温度对 NPP 的贡献大于其他月份,7 月的降水对 NPP 的影响大于其他月份;(3)气候因子导致长江源区大部分地区的 NPP 增加。人类活动的影响主要集中在下游地区,是导致 NPP 下降的主要原因。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8eae/7809463/ce338e59247a/41598_2020_80494_Fig1_HTML.jpg

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