LI Xiaoli, CAO Min, MAO Yang. Variation Characteristics and Influencing Factors of NDVI in Karst Trough Area of Southwest China in Recent 20 Years Based on Ggeo-detector[J]. 2021, 35(6): 38-44.
DOI:
LI Xiaoli, CAO Min, MAO Yang. Variation Characteristics and Influencing Factors of NDVI in Karst Trough Area of Southwest China in Recent 20 Years Based on Ggeo-detector[J]. 2021, 35(6): 38-44. DOI: 10.13870/j.cnki.stbcxb.2021.06.006.
Variation Characteristics and Influencing Factors of NDVI in Karst Trough Area of Southwest China in Recent 20 Years Based on Ggeo-detector
The study on the change of vegetation coverage and its relationship with the driving factors is the basis of benefit evaluation on large-scale vegetation restoration
but the spatial-temporal change patterns of vegetation and its driving factors in the southwest karst trough-valley region are still not clear at present
which is not conducive to further ecological construction. This study explored the spatio-temporal characteristics and driving factors of vegetation coverage change based on the data of NDVI
air temperature
rainfall
DEM
land cover and population density in the southwest trough valley area from 2000 to 2018 and to predict the future trends. The methods of linear trend regression analysis and Hurst index analysis as well as the geographic detector model were applied. The results showed that: (1) In recent 19 years
the range of NDVI was 0.785~0.838
which showed a fluctuating upward trend
and the annual growth rate of vegetation NDVI (0.003 17/a) in karst area was significantly higher than that in non-karst area (0.002 60/a). (2) Hurst index analysis showed that the vegetation NDVI in the study area mainly showed an upward trend
but 64.31% of them would show a degradation trend in the future
and the situation of vegetation protection was more severe. (3) There was a negative correlation between NDVI and temperature change (R=-0.040) in karst area
but a positive correlation (R=0.013) in non-karst area. The results of residual analysis showed that human activities promoted the NDVI growth of 89.60% of regional vegetation. (4) In the whole karst trough-valley area
land cover type and air temperature were the main driving factors affecting NDVI
the interpretation rate was over 25%
and the interaction of each factor was obviously higher than that of a single factor. On the whole
human activities had a significant positive impact on the vegetation restoration in the southwest trough valley area.
Piao S P S, Yin G Y G, Tan J G, et al. Detection and attribution of vegetation greening trend in China over the last 30years[J].Global Change Biology, 2015, 21(4):1601-1609.
Brandt M, Yue Y, Wigneron J P, et al. Satellite-observed major greening and 448 biomass increase in South China Karst during recent decade[J].Earth's Future, 2018, 6:1017-1028.
Qiao Y N, Jiang Y J, Zhang C Y. Contribution of karst ecological restoration engineering to vegetation greening in southwest China during recent decade[J].Ecological Indicators, 2021, 121:e107081.
Chai Z. Soil erosion in karst areas of Guangxi[J].Journal of Mountain Research, 1989, 7(4):255-260.
Wang S J, Liu Q M, Zhang D F. Karst rocky desertification in southwestern China:Geomorphology, landuse, impact and rehabilitation[J].Land Degradation and Development, 2010, 15(2):115-121.
Zhou Q W, Luo Y, Zhou X, et al. Response of vegetation to water balance conditions at different time scales across the karst area of southwestern China:A remote sensing approach[J]. Science of the Total Environment, 2018, 645:460-470.