Zhao Wenbo, Feng Lili, Zhao Anzhou, et al. Spatial and Temporal Evolution of Desertification and Its Driving Factors of Climate in Hebei Province[J]. Bulletin of Soiland Water Conservation, 2021, 41(4): 252-259.
DOI:
Zhao Wenbo, Feng Lili, Zhao Anzhou, et al. Spatial and Temporal Evolution of Desertification and Its Driving Factors of Climate in Hebei Province[J]. Bulletin of Soiland Water Conservation, 2021, 41(4): 252-259. DOI: 10.13961/j.cnki.stbctb.2021.04.034.
Spatial and Temporal Evolution of Desertification and Its Driving Factors of Climate in Hebei Province
[Objective] The desertification in Hebei Province was monitored by remote sensing and its driving factors was analyzed
in order to provide reliable theoretical basis and data support for desertification control. [Methods] Based on MODIS13 A3-NDVI and meteorological data from 2000 to 2017
taking the desertification index as the evaluation index
the temporal and spatial evolution of land desertification in Hebei Province and its driving factors were analyzed by trend analysis
future change analysis
and climate factors analysis. [Results] ① In 2000—2017
the desertification of study area decreased
with a decreasing rate of 0.009/18 a
of which the proportion of extremely significant decrease (p<0.01) was 11.13% and significant decrease (p<0.05) was 8.86%. ② The proportions of persistent and anti-persistent desertification in future in the study area were expected to be 41.29% and 58.71% respectively
of which
the weak persistence and weak anti-persistence was expected to be 37.43% and 51.35%
respectively. On the existing basis
the trend change in the future was basically unchanged
and the proportions of persistent and anti-persistent characteristics were 14.89% and 19.6% respectively. ③ The partial correlation coefficient of desertification index with precipitation and temperature in growing season was small and insignificant. [Conclusion] The overall desertification situation is improved during 2000—2017
but with obvious spatial heterogeneity. The desertification areas are mainly concentrated in the Bashang Plateau area and the Hurst index indicates that desertification might be reversed in local areas in the future. In terms of climate factors
the increase of temperature and the decrease of precipitation can promote desertification in the study area.
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