Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011

In this study, two different methods including Digital Camera and Reference Panel (DCRP) and traditional in situ fPAR observation for measuring the in situ point fPAR of very short alpine grass vegetation were compared, and the Moderate Resolution Imaging Spectroradiometer (MODIS) fPAR products were...

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Main Authors: Bao-Xiong Chen, Xian-Zhou Zhang, Yu-Fang Sun, Jing-Sheng Wang, Yong-Tao He
Format: Article
Language:English
Published: KeAi Communications Co., Ltd. 2017-06-01
Series:Advances in Climate Change Research
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674927816300740
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author Bao-Xiong Chen
Xian-Zhou Zhang
Yu-Fang Sun
Jing-Sheng Wang
Yong-Tao He
author_facet Bao-Xiong Chen
Xian-Zhou Zhang
Yu-Fang Sun
Jing-Sheng Wang
Yong-Tao He
author_sort Bao-Xiong Chen
collection DOAJ
description In this study, two different methods including Digital Camera and Reference Panel (DCRP) and traditional in situ fPAR observation for measuring the in situ point fPAR of very short alpine grass vegetation were compared, and the Moderate Resolution Imaging Spectroradiometer (MODIS) fPAR products were evaluated and validated by in situ point data on the alpine grassland over the Northern Tibetan Plateau, which is sensitive to climate change and vulnerable to anthropogenic activities. Results showed that the MODIS alpine grassland fPAR product, examined by using DCRP, and traditional in situ fPAR observation had a significant relationship at the spatial and temporal scales. The decadal MODIS fPAR trend analysis showed that, average growing season fPAR increased by 1.2 × 10−4 per year and in total increased 0.86% from 2002 to 2011 in alpine grassland, when most of the fPAR increments occurred in southeast and center of the Northern Tibetan Plateau, the alpine grassland tended to recover from degradation slightly. However, climatic factors have influenced the various alpine grassland vegetation fPAR over a period of 10 years; precipitation significantly affected the alpine meadow fPAR in the eastern region, whereas temperature considerably influenced the alpine desert steppe fPAR in the west region. These findings suggest that the regional heterogeneity in alpine grassland fPAR results from various environmental factors, except for vegetation characteristics, such as canopy structure and leaf area.
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spelling doaj.art-7812667c9e704d498748b450808b096e2022-12-21T19:59:27ZengKeAi Communications Co., Ltd.Advances in Climate Change Research1674-92782017-06-018210811610.1016/j.accre.2017.05.008Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011Bao-Xiong Chen0Xian-Zhou Zhang1Yu-Fang Sun2Jing-Sheng Wang3Yong-Tao He4Rural Energy & Environment Agency, Ministry of Agriculture of the People's Republic of China, Beijing 100125, ChinaLhasa Plateau Ecosystem Research Station, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Science, Beijing 100101, ChinaRural Energy & Environment Agency, Ministry of Agriculture of the People's Republic of China, Beijing 100125, ChinaLhasa Plateau Ecosystem Research Station, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Science, Beijing 100101, ChinaLhasa Plateau Ecosystem Research Station, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Science, Beijing 100101, ChinaIn this study, two different methods including Digital Camera and Reference Panel (DCRP) and traditional in situ fPAR observation for measuring the in situ point fPAR of very short alpine grass vegetation were compared, and the Moderate Resolution Imaging Spectroradiometer (MODIS) fPAR products were evaluated and validated by in situ point data on the alpine grassland over the Northern Tibetan Plateau, which is sensitive to climate change and vulnerable to anthropogenic activities. Results showed that the MODIS alpine grassland fPAR product, examined by using DCRP, and traditional in situ fPAR observation had a significant relationship at the spatial and temporal scales. The decadal MODIS fPAR trend analysis showed that, average growing season fPAR increased by 1.2 × 10−4 per year and in total increased 0.86% from 2002 to 2011 in alpine grassland, when most of the fPAR increments occurred in southeast and center of the Northern Tibetan Plateau, the alpine grassland tended to recover from degradation slightly. However, climatic factors have influenced the various alpine grassland vegetation fPAR over a period of 10 years; precipitation significantly affected the alpine meadow fPAR in the eastern region, whereas temperature considerably influenced the alpine desert steppe fPAR in the west region. These findings suggest that the regional heterogeneity in alpine grassland fPAR results from various environmental factors, except for vegetation characteristics, such as canopy structure and leaf area.http://www.sciencedirect.com/science/article/pii/S1674927816300740fPARAlpine grasslandMODISNorthern Tibetan PlateauClimate change
spellingShingle Bao-Xiong Chen
Xian-Zhou Zhang
Yu-Fang Sun
Jing-Sheng Wang
Yong-Tao He
Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
Advances in Climate Change Research
fPAR
Alpine grassland
MODIS
Northern Tibetan Plateau
Climate change
title Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
title_full Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
title_fullStr Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
title_full_unstemmed Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
title_short Alpine grassland fPAR change over the Northern Tibetan Plateau from 2002 to 2011
title_sort alpine grassland fpar change over the northern tibetan plateau from 2002 to 2011
topic fPAR
Alpine grassland
MODIS
Northern Tibetan Plateau
Climate change
url http://www.sciencedirect.com/science/article/pii/S1674927816300740
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AT yufangsun alpinegrasslandfparchangeoverthenortherntibetanplateaufrom2002to2011
AT jingshengwang alpinegrasslandfparchangeoverthenortherntibetanplateaufrom2002to2011
AT yongtaohe alpinegrasslandfparchangeoverthenortherntibetanplateaufrom2002to2011