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Analysis of the Spatio-temporal Variation in FPAR of the Tibetan Plateau from 1982 to 2015 |
Xuemin Jiao1,2(),Helin Zhang5,Fubao Xu6,Yan Wang2,Dailiang Peng2,Cunjun Li3,Xiyan Xu4,Haisheng Fan7,Yunxin Huang1() |
1.College of Resources and Environmental Sciences, Hubei University, Hubei Key Laboratory of Regional Development and Environmental Response, Wuhan 430062, China 2.Digital Earth Key Laboratory, Institute of Remote Sensing and Digital Earth Chinese Academy of Sciences, Beijing 100094, China 3.National Agricultural Information Engineering Research Center,Beijing Academy of Agricultural and Forestry Sciences,Beijing 100097, China 4.Institute of atmospheric physics, Chinese Academy of Sciences, Beijing 100029, China 5.Facultv of Geoarphical Science BNU, Beijing Normal University, Beijing 100875, China 6.Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China 7.Department of Satellite Big Data Business, Zhuhai Orbita Aerospace Science & Technology Co. , ltd. , Zhuhai 519080, China |
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Abstract The absorbed and utilized Fraction of Photosynthetically Active Radiation(FPAR) reflects the capacity of carbon fixation and oxygen release by vegetation, which may vary over space and time in large scale. Analysis of spatial-temporal variation in FPAR is an important topic of plant ecology. Based on GIMMS NDVI3g (1982~2015) and MODIS NDVI (2001~2015) data in the Tibetan plateau, here we used the nonlinear, semi-theoretical and semi-empirical models to inverse and analyze the spatial and temporal variation in FPAR. The results showed that (1) The spatial distributions of FPAR derived from GIMMS NDVI3g and MODIS NDVI were highly consistent, with the correlation coefficient being 0.82 (P<0.01). The area in which the trends of inter-annual change in the two inversion data were consistent for at least 6 years made up 80% of the studying area. (2) FPAR in Tibetan Plateau was greatly affected by slope and altitude. Changes in FPAR were fastest at slopes of 15~35 degrees and highest at altitude of 700~2 100 m. The effect of slope direction on FPAR was limited. There was little difference in FPAR among different slope directions except for the south where the FPAR was relatively lower. (3)The FPAR data from 1982 to 2015 demonstrated seasonal variation. The inter-annual variation in FPAR was most significant in winter, in which FPAR in about 78.5% of the area increased. FPAR declined most significantly in the fall. (4) FPAR derived from both the MODIS NDVI and GIMMS NDVI data demonstrated a small, temporary decline in 2012. The trend of inter-annual variation in FPAR was largely different among different vegetation types. In conclusion, the FPAR data from 1982 to 2015 in the Tibetan plateau demonstrated both spatial and seasonal variation, which may have important implications for further studies concerning climate and environmental changes in the region.
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Received: 31 May 2019
Published: 15 September 2020
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Corresponding Authors:
Yunxin Huang
E-mail: Jiaoxm1117@163.com;y.huang@hubu.edu.cn
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Cite this article:
Xuemin Jiao,Helin Zhang,Fubao Xu,Yan Wang,Dailiang Peng,Cunjun Li,Xiyan Xu,Haisheng Fan,Yunxin Huang. Analysis of the Spatio-temporal Variation in FPAR of the Tibetan Plateau from 1982 to 2015. Remote Sensing Technology and Application, 2020, 35(4): 950-961.
URL:
http://www.rsta.ac.cn/EN/10.11873/j.issn.1004-0323.2020.4.0950 OR http://www.rsta.ac.cn/EN/Y2020/V35/I4/950
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