Spatio-temporal dynamics of NDVI and its response to climate factors in the Heihe River Basin, China
Ecosystem in the Heihe River Basin (HRB) is very vulnerable and sensitive to variations in the climatic conditions and human activities. In this study, The SPOT and MODIS NDVI time series data from 1998 to 2012 were used to analyze NDVI variation characteristics and its response to climatic factors...
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description | Ecosystem in the Heihe River Basin (HRB) is very vulnerable and sensitive to variations in the climatic conditions and human activities. In this study, The SPOT and MODIS NDVI time series data from 1998 to 2012 were used to analyze NDVI variation characteristics and its response to climatic factors in the HRB based on Mann-Kendall test, relative Sen's slope, linear regression and partial correlation analysis. The results indicate that: (1) There is an obvious decreasing trend during 1998-2001 and a significantly increasing trend from 2001 to 2012. The vegetation in the HRB was improved by 1.5% of annual average level from 1998 to 2012, and rate of change is greatest in the lower reaches. (2) During 1998-2001, the rainfall is proved to be the most significant factor influencing NDVI for each reaches, and temperature and radiation are also related significantly with NDVI in the middle and lower reaches respectively. However, during 2001-2012, all climatic factors are not significantly related with NDVI for each reaches, excepting rainfall in the middle reaches. This demonstrates that the climatic variation cannot totally explain the significant improvement of vegetation during 2001-2012 in the HRB, whereas ecological restoration projects implemented in this period might be a reasonable factor for the improvement of ecological environment in the HRB. |
doi_str_mv | 10.1088/1755-1315/82/1/012045 |
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In this study, The SPOT and MODIS NDVI time series data from 1998 to 2012 were used to analyze NDVI variation characteristics and its response to climatic factors in the HRB based on Mann-Kendall test, relative Sen's slope, linear regression and partial correlation analysis. The results indicate that: (1) There is an obvious decreasing trend during 1998-2001 and a significantly increasing trend from 2001 to 2012. The vegetation in the HRB was improved by 1.5% of annual average level from 1998 to 2012, and rate of change is greatest in the lower reaches. (2) During 1998-2001, the rainfall is proved to be the most significant factor influencing NDVI for each reaches, and temperature and radiation are also related significantly with NDVI in the middle and lower reaches respectively. However, during 2001-2012, all climatic factors are not significantly related with NDVI for each reaches, excepting rainfall in the middle reaches. This demonstrates that the climatic variation cannot totally explain the significant improvement of vegetation during 2001-2012 in the HRB, whereas ecological restoration projects implemented in this period might be a reasonable factor for the improvement of ecological environment in the HRB.</description><identifier>ISSN: 1755-1307</identifier><identifier>EISSN: 1755-1315</identifier><identifier>DOI: 10.1088/1755-1315/82/1/012045</identifier><language>eng</language><publisher>Bristol: IOP Publishing</publisher><subject>Aquatic ecosystems ; Climatic conditions ; Correlation analysis ; Environmental restoration ; Radiation ; Rainfall ; River basins ; Rivers ; Variation ; Vegetation</subject><ispartof>IOP conference series. Earth and environmental science, 2017-08, Vol.82 (1), p.12045</ispartof><rights>Published under licence by IOP Publishing Ltd</rights><rights>2017. This work is published under http://creativecommons.org/licenses/by/3.0/ (the “License”). 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Earth and environmental science</title><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><description>Ecosystem in the Heihe River Basin (HRB) is very vulnerable and sensitive to variations in the climatic conditions and human activities. In this study, The SPOT and MODIS NDVI time series data from 1998 to 2012 were used to analyze NDVI variation characteristics and its response to climatic factors in the HRB based on Mann-Kendall test, relative Sen's slope, linear regression and partial correlation analysis. The results indicate that: (1) There is an obvious decreasing trend during 1998-2001 and a significantly increasing trend from 2001 to 2012. The vegetation in the HRB was improved by 1.5% of annual average level from 1998 to 2012, and rate of change is greatest in the lower reaches. (2) During 1998-2001, the rainfall is proved to be the most significant factor influencing NDVI for each reaches, and temperature and radiation are also related significantly with NDVI in the middle and lower reaches respectively. However, during 2001-2012, all climatic factors are not significantly related with NDVI for each reaches, excepting rainfall in the middle reaches. This demonstrates that the climatic variation cannot totally explain the significant improvement of vegetation during 2001-2012 in the HRB, whereas ecological restoration projects implemented in this period might be a reasonable factor for the improvement of ecological environment in the HRB.</description><subject>Aquatic ecosystems</subject><subject>Climatic conditions</subject><subject>Correlation analysis</subject><subject>Environmental restoration</subject><subject>Radiation</subject><subject>Rainfall</subject><subject>River basins</subject><subject>Rivers</subject><subject>Variation</subject><subject>Vegetation</subject><issn>1755-1307</issn><issn>1755-1315</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>O3W</sourceid><sourceid>BENPR</sourceid><recordid>eNqFUMFKAzEUDKJgrX6CEPDgxXXzdjeb7FFrtQVRsOo1pEmWprSbNUmF_r1bVqoHwct7j2FmHjMInQO5BsJ5CozSBHKgKc9SSAlkpKAHaLDHD_c3YcfoJIQlISUr8mqA9KyV0bokmnXrvFxhvW3k2qqAXY2f7t6nWDYa2xiwN6F1TTA4OqxWdi2jwbVU0fmAbYPjwuCJsd18sZ_G41sZbHOFRwvbyFN0VMtVMGffe4je7sevo0ny-PwwHd08JqqgJCa0oPNSc9DVnEFlIFdUkwwKxhVnfJ7JqsgIV5SV2hCoqrIk1KgOZmVWK1PlQ3TR-7befWxMiGLpNr7pXoqMlgRyBl3qIaI9S3kXgje1aH0Xx28FELErVOzKErviBM8EiL7QTge9zrr2x_g_zeUfmvF49pslWl3nX_RYgi0</recordid><startdate>20170801</startdate><enddate>20170801</enddate><creator>Cheng, C X</creator><creator>Wang, Z H</creator><creator>Xiao, P Q</creator><creator>Xu, Z X</creator><creator>Jiao, P</creator><creator>Dong, G T</creator><creator>Wei, G J</creator><general>IOP Publishing</general><scope>O3W</scope><scope>TSCCA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>PATMY</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope></search><sort><creationdate>20170801</creationdate><title>Spatio-temporal dynamics of NDVI and its response to climate factors in the Heihe River Basin, China</title><author>Cheng, C X ; Wang, Z H ; Xiao, P Q ; Xu, Z X ; Jiao, P ; Dong, G T ; Wei, G J</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c450t-545b6d81d9b719e13c5d021478c878b2a94208c576de01996605ec2a9762fce93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Aquatic ecosystems</topic><topic>Climatic conditions</topic><topic>Correlation analysis</topic><topic>Environmental restoration</topic><topic>Radiation</topic><topic>Rainfall</topic><topic>River basins</topic><topic>Rivers</topic><topic>Variation</topic><topic>Vegetation</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Cheng, C X</creatorcontrib><creatorcontrib>Wang, Z H</creatorcontrib><creatorcontrib>Xiao, P Q</creatorcontrib><creatorcontrib>Xu, Z X</creatorcontrib><creatorcontrib>Jiao, P</creatorcontrib><creatorcontrib>Dong, G T</creatorcontrib><creatorcontrib>Wei, G J</creatorcontrib><collection>Institute of Physics Open Access Journal Titles</collection><collection>IOPscience (Open Access)</collection><collection>CrossRef</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>Environmental Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Environmental Science Collection</collection><jtitle>IOP conference series. Earth and environmental science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Cheng, C X</au><au>Wang, Z H</au><au>Xiao, P Q</au><au>Xu, Z X</au><au>Jiao, P</au><au>Dong, G T</au><au>Wei, G J</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatio-temporal dynamics of NDVI and its response to climate factors in the Heihe River Basin, China</atitle><jtitle>IOP conference series. Earth and environmental science</jtitle><addtitle>IOP Conf. Ser.: Earth Environ. Sci</addtitle><date>2017-08-01</date><risdate>2017</risdate><volume>82</volume><issue>1</issue><spage>12045</spage><pages>12045-</pages><issn>1755-1307</issn><eissn>1755-1315</eissn><abstract>Ecosystem in the Heihe River Basin (HRB) is very vulnerable and sensitive to variations in the climatic conditions and human activities. In this study, The SPOT and MODIS NDVI time series data from 1998 to 2012 were used to analyze NDVI variation characteristics and its response to climatic factors in the HRB based on Mann-Kendall test, relative Sen's slope, linear regression and partial correlation analysis. The results indicate that: (1) There is an obvious decreasing trend during 1998-2001 and a significantly increasing trend from 2001 to 2012. The vegetation in the HRB was improved by 1.5% of annual average level from 1998 to 2012, and rate of change is greatest in the lower reaches. (2) During 1998-2001, the rainfall is proved to be the most significant factor influencing NDVI for each reaches, and temperature and radiation are also related significantly with NDVI in the middle and lower reaches respectively. However, during 2001-2012, all climatic factors are not significantly related with NDVI for each reaches, excepting rainfall in the middle reaches. 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subjects | Aquatic ecosystems Climatic conditions Correlation analysis Environmental restoration Radiation Rainfall River basins Rivers Variation Vegetation |
title | Spatio-temporal dynamics of NDVI and its response to climate factors in the Heihe River Basin, China |
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