Variations and Impact Factors of NDVI in Dulan County of Qinghai Provinc
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Variations and Impact Factors of NDVI in Dulan County of Qinghai Provinc
Bulletin of Soiland Water ConservationVol. 30, Issue 5, Pages: 204-207(2011)
作者机构:
北京林业大学水土保持学院水土保持与荒漠化防治教育部重点实验室
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Published:2011
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Chang Jin, Zhang Ke-bin, Bian Zhen, et al. Variations and Impact Factors of NDVI in Dulan County of Qinghai Provinc[J]. Bulletin of Soiland Water Conservation, 2011, 30(5): 204-207.
DOI:
Chang Jin, Zhang Ke-bin, Bian Zhen, et al. Variations and Impact Factors of NDVI in Dulan County of Qinghai Provinc[J]. Bulletin of Soiland Water Conservation, 2011, 30(5): 204-207.DOI:
Variations and Impact Factors of NDVI in Dulan County of Qinghai Provinc
The knowledge of vegetation cover changes will provide considerable insights into the dynamic process of desertification.The study illustrated the vegetation dynamic changes in Dulan County
Qinghai Province using 2000—2009MODIS NDVI data
and on this basis
the relationship between NDVI changes with temperature and rainfall variations were investigated
providing the basic data to land use planning in alpine areas and desertification prevention and control.The results indicate that the NDVI values of the area presented a slow ascendant trend from 2000to 2009
at the rate of 0.002 9/a.The NDVI values had a strong seasonal changes in a year
but the overall NDVIs were not high for the county
with the maximum value of 0.22.The vegetation condition were improved significantly in 39.71%of the area of the entire county
which mainly located in basins of Chacha river and Chahanwusu river and a large area of Qaidam river downstream.However
the vegetation degeneration was found in the upper and middle reaches of Qaidam river
accounting for 17.74%of the entire county
suggesting that the desertification control should be further strengthened.The temperature and rainfall were the two main natural factors influencing the NDVI dynamics of the county;the NDVIs correlated strongly significantly with the temperature(p< 0.01)
and significantly with the rainfall amount(p<0.05)from May to September annually.The impact of the temperature on the NDVI was stronger than that of the precipitation