长江流域资源与环境 >> 2023, Vol. 32 >> Issue (10): 2137-2146.doi: 10.11870/cjlyzyyhj202310012

• 自然资源 • 上一篇    下一篇

不同气候区流域植被净初级生产力空间特征及驱动因子对比研究

徐颖 1,2,3,朱青2,3*,王国杰1,王永武2,3   

  1. (1.南京信息工程大学地理科学学院,江苏 南京 210044;2.中国科学院南京地理与湖泊研究所,中国科学院流域地理学重点实验室,江苏 南京 210008;3.中国科学院大学,北京 100049)
  • 出版日期:2023-10-20 发布日期:2023-10-26

A Comparative Study on the Spatial Characteristics and Drivers of Net Primary  Productivity of Vegetation in Watersheds of Different Climatic Zones

XU Ying1,2,3,ZHU Qing2,3,WANG Guo-jie1,WANG Yong-wu2,3   

  1. (1.School of Geographical Sciences,Nanjing University of Information Science and Technology,Nanjing 210044,China;2.Key Laboratory of Watershed Geographic Sciences, Nanjing Institute of Geography and Limnology,Chinese Academy of Sciences,Nanjing 210008,China; 3.University of Chinese Academy of Sciences,Beijing 100049,China)
  • Online:2023-10-20 Published:2023-10-26

摘要: 植被净初级生产力(NPP)是地表碳循环的重要组成部分,对于全球气候变化和碳平衡具有重要意义。基于CASA模型,计算并对比分析了2010~2019年黑河流域、渭河流域和长江下游流域植被NPP空间变化规律与主控因子,结果表明:(1)湿润区流域(长江下游流域)的植被NPP值和增长速率明显高于干旱区和半干旱区流域(黑河流域和渭河流域);(2)不同土地覆盖类型面积和单位面积NPP值,是决定3个流域植被NPP空间分布的主导因素,黑河流域植被NPP贡献最大的是草地和未利用地,而渭河流域和长江下游流域NPP总量最大的是草地和农田;(3)不同流域植被NPP空间分布随高程和坡度变化的规律不同,但其随年均气温和降水的升高均呈现先增后减趋势;(4)渭河流域植被NPP受气象因子交互作用强,长江下游流域植被NPP受地形因子交互作用强,而黑河流域植被NPP受二者的影响相近。研究结果识别不同气候区植被NPP变化的主控因素和精确估算陆地生态系统的固碳潜力具有重要意义。


Abstract: Net Primary Productivity (NPP) of vegetation is a critical component of the terrestrial carbon cycle, and plays an important rolein global climate change and carbon equilibrium. Based on the CASA model, this study calculated and compared the spatial variations and key controlling factors of NPP in the Heihe River Basin, Weihe River Basin, and the lower reach of Yangtze River Basin from 2010 to 2019. These three basins represented the arid, semi-arid and humid zones, respectively. Results indicated that:(1) The NPP value and its increasing rate in the lower reach of Yangtze River Basin wereobviously higher than those in the Heihe River Basin and Weihe River Basin.(2)The area proportions and areal mean NPP values of different land cover types were the dominant factors determining the spatial patterns of NPP in the three basins. Grassland and the unutilized land had the greatest contributions to the NPP in the Heihe River Basin, while grassland and farmland contributed the most to the total NPP in both the Weihe River Basin and the lower reach of Yangtze River Basin. (3) The spatial patterns of NPP in different basins variedaccording to thespatial patterns of elevation and slope. However, similar increasing and then decreasing trend of the NPP with the increasing of annual mean temperature and precipitation were also observed in these three basins.(4) The NPP in the Weihe River Basin was primarily influenced by the meteorological factors, while that in the lower reach of Yangtze River Basin was strongly influenced by the terrain factors, and in the Heihe River Basin, the meteorological and terrain factors had similar effects on the NPP. These results are of significant importance for identifying the main controlling factors of vegetation NPP changes in different climatic regions and for estimating  the carbon sequestration potential of terrestrial ecosystems.


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