2021
DOI: 10.1002/ldr.4129
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Satellite remote sensing analysis to monitor revegetation in the Yangtze River basin, China

Abstract: Revegetation programmes aim to avoid land degradation, control soil erosion, reduce floods, and improve ecological conditions. China has planted billions of trees over the past 20 years. However, little is known about the effectiveness of this artificial revegetation and its consequences on China's national conservation policies and changes in biophysical factors at the county level. Here we use satellite time series data and develop a new metric, the revegetation index (RVI), that quickly monitors revegetatio… Show more

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Cited by 3 publications
(2 citation statements)
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References 40 publications
(39 reference statements)
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“…To obtain an annual consistent NDVI data with high spatiotemporal resolution from 1982 to 2011, we downscaled the coarse‐resolution (8000 m × 8000 m) to medium spatial resolution (250 m × 250 m) (hereafter, NDVI‐ESTARFM) using ESTARFM algorithm (Zhu et al, 2010). It has been validated by the example of Yangtze River basin (Li, Wang, et al, 2021), which showed that the NDVI‐ESTARFM datasets calculated by this method are consistent with the actual NDVI data. The equation is expressed as follows: (Fx,y,tp,B)=(Fx,y,t0,B)+vx,y×Cx,y,tp,BCx,y,t0,B Where : F and C represent the fine‐resolution reflectance at base date t0 for band B and coarse‐ resolution reflectance at prediction data tp for band B, respectively, (x,y) is the location for both fine‐ and coarse‐resolution images, t0 and tp is the acquisition date, vx,y stands for the conversion coefficient by linearly regressing the reflectance changes of fine‐resolution pixels of the same endmember and coarse‐ resolution pixel.…”
Section: Methodsmentioning
confidence: 75%
See 1 more Smart Citation
“…To obtain an annual consistent NDVI data with high spatiotemporal resolution from 1982 to 2011, we downscaled the coarse‐resolution (8000 m × 8000 m) to medium spatial resolution (250 m × 250 m) (hereafter, NDVI‐ESTARFM) using ESTARFM algorithm (Zhu et al, 2010). It has been validated by the example of Yangtze River basin (Li, Wang, et al, 2021), which showed that the NDVI‐ESTARFM datasets calculated by this method are consistent with the actual NDVI data. The equation is expressed as follows: (Fx,y,tp,B)=(Fx,y,t0,B)+vx,y×Cx,y,tp,BCx,y,t0,B Where : F and C represent the fine‐resolution reflectance at base date t0 for band B and coarse‐ resolution reflectance at prediction data tp for band B, respectively, (x,y) is the location for both fine‐ and coarse‐resolution images, t0 and tp is the acquisition date, vx,y stands for the conversion coefficient by linearly regressing the reflectance changes of fine‐resolution pixels of the same endmember and coarse‐ resolution pixel.…”
Section: Methodsmentioning
confidence: 75%
“…The equation is expressed as follows: (Fx,y,tp,B)=(Fx,y,t0,B)+vx,y×Cx,y,tp,BCx,y,t0,B Where : F and C represent the fine‐resolution reflectance at base date t0 for band B and coarse‐ resolution reflectance at prediction data tp for band B, respectively, (x,y) is the location for both fine‐ and coarse‐resolution images, t0 and tp is the acquisition date, vx,y stands for the conversion coefficient by linearly regressing the reflectance changes of fine‐resolution pixels of the same endmember and coarse‐ resolution pixel. Details of the derivation of ESTARFM can be found in Zhu et al (2010) and Li, Wang, et al (2021).…”
Section: Methodsmentioning
confidence: 99%