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[1999 - 2015年若尔盖草原湿地净初级生产力的时空变化]

[Spatio-temporal variation of NPP from 1999 to 2015 in Zoige grassland wetland, China].

作者信息

Guo Bin, Wang Shan, Wang Ming-Tian

机构信息

Sichuan Province Key Laboratory of Heavy Rain and Drought-Flood Disasters in Plateau and Basin, Chengdu 610072, China.

Aba Prefecture Meteorological Station, Maerkang 624000, Sichuan, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2020 Feb;31(2):424-432. doi: 10.13287/j.1001-9332.202002.018.

DOI:10.13287/j.1001-9332.202002.018
PMID:32476334
Abstract

Net primary productivity (NPP) is one of the core components of the grassland wetland ecosystem carbon balance and climate change. Based on data of vegetation index, meteorology (precipitation and temperature), and vegetation type, we used the CASA (Carnegie-Ames-Stanford Approach) model to estimate NPP of the Zoige grassland wetland from 1999 to 2015. The spatial and temporal patterns of NPP in the Zoige grassland wetland ecological function area and its relationship with precipitation and temperature were examined. The results showed that the measured values of NPP were close to the simulated values, with the root mean square error being 120.3 g C·m and a R of 0.78. The annual mean and the growth season (April-September) mean of NPP of the study area were 329.0 and 229.4 g C·m·a, respectively, with obvious inter-annual fluctuations, with a weak trend of decline (2.3, 1.6 g C·m·a). The inter-annual fluctuations of NPP in different vegetation types were basically consistent with the overall fluctuations of NPP of the whole study area. The slope of NPP in annual and growing seasons was from -21.3 to 18.7, -31.5 to 23.1 g C·m·a. The area with significant increase (mainly distributed in forest coverage area and wetland ecological compensation area) only accouned for 0.3% and 0.7% of the total area, and the area with significant decline (mainly distributed in areas where human activities were concentrated) only accounted for 1.4% and 6.4% of the total area, respectively. The carbon sequestration capacity of different vegetation types was different, among which the forest was the strongest, the grassland was the second, and the wetland vegetation was the weakest. Precipitation was the dominant climatic factor affecting NPP in grassland wetland.

摘要

净初级生产力(NPP)是草地湿地生态系统碳平衡和气候变化的核心组成部分之一。基于植被指数、气象数据(降水量和温度)以及植被类型数据,我们使用CASA(卡内基-埃姆斯-斯坦福方法)模型估算了1999年至2015年若尔盖草地湿地的NPP。研究了若尔盖草地湿地生态功能区NPP的时空格局及其与降水量和温度的关系。结果表明,NPP实测值与模拟值接近,均方根误差为120.3 g C·m ,相关系数R为0.78。研究区NPP的年平均值和生长季(4月至9月)平均值分别为329.0和229.4 g C·m·a,年际波动明显,呈微弱下降趋势(2.3、1.6 g C·m·a)。不同植被类型NPP的年际波动与整个研究区NPP的总体波动基本一致。年和生长季NPP的斜率分别为-21.3至18.7、-31.5至23.1 g C·m·a。显著增加的区域(主要分布在森林覆盖区和湿地生态补偿区)仅占总面积的0.3%和0.7%,显著下降的区域(主要分布在人类活动集中的区域)分别仅占总面积的1.4%和6.4%。不同植被类型的碳固存能力不同,其中森林最强,草地次之,湿地植被最弱。降水量是影响草地湿地NPP的主要气候因子。

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