2021
DOI: 10.1007/s10661-021-09078-y
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Soil moisture change analysis under watershed management practice using in situ and remote sensing data in a paired watershed

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Cited by 4 publications
(5 citation statements)
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“…The upper and lower thresholds of land surface temperature are represented on both sides of the characteristic space, and the calculated TVDI values are subsequently used to infer the degree of drought, which can more accurately determine the SM. A significant negative correlation was found between the TVDI and SM in different arid and semi-arid regions (Guo et al, 2009; Rev Bras Cienc Solo 2022;46:e0220113 Kazemzadeh et al, 2021). Due to the discrepancies in climate and soil environment in different regions, the feature space (Vis-TVDI) and LST that constitute the TVDI were modified in a suitable manner, summarized as follows: (a) replaced NDVI and used the modified soil adjusted VI (MSAVI), soil adjusted VI (SAVI), and enhanced VI (EVI) for evaluation (Zhang et al, 2014a;Ma et al, 2017;Wu et al, 2019); (b) modified the soil line and increased the combination of shortwave infrared (SWIR), near-infrared (NIR), and red light bands to reduce the sensitivity of VI to the soil background (Feng et al, 2011a;Chen et al, 2019;Liu et al, 2021b); (c) considered the influence of factors such as terrain (digital elevation model, DEM) and environmental data on the LST and made corrections to the LST (Ran et al, 2005;Sun et al, 2010;Liu et al, 2013).…”
Section: Introductionmentioning
confidence: 93%
“…The upper and lower thresholds of land surface temperature are represented on both sides of the characteristic space, and the calculated TVDI values are subsequently used to infer the degree of drought, which can more accurately determine the SM. A significant negative correlation was found between the TVDI and SM in different arid and semi-arid regions (Guo et al, 2009; Rev Bras Cienc Solo 2022;46:e0220113 Kazemzadeh et al, 2021). Due to the discrepancies in climate and soil environment in different regions, the feature space (Vis-TVDI) and LST that constitute the TVDI were modified in a suitable manner, summarized as follows: (a) replaced NDVI and used the modified soil adjusted VI (MSAVI), soil adjusted VI (SAVI), and enhanced VI (EVI) for evaluation (Zhang et al, 2014a;Ma et al, 2017;Wu et al, 2019); (b) modified the soil line and increased the combination of shortwave infrared (SWIR), near-infrared (NIR), and red light bands to reduce the sensitivity of VI to the soil background (Feng et al, 2011a;Chen et al, 2019;Liu et al, 2021b); (c) considered the influence of factors such as terrain (digital elevation model, DEM) and environmental data on the LST and made corrections to the LST (Ran et al, 2005;Sun et al, 2010;Liu et al, 2013).…”
Section: Introductionmentioning
confidence: 93%
“…In recent decades, remote sensing techniques have been developed to estimate soil moisture (Moran et al, 2004;Amani et al, 2016;Mohamed et al, 2020;Kazemzadeh et al, 2021;). Radiation including nearinfrared (NIR), visible light (VIS), thermal infrared (TIR), soil moisture ocean salinity (SMOS), short wave infrared (SWIR) reflectance, soil moisture active passive (SMAP), and microwave are used to retrieve soil moisture data from the topsoil.…”
Section: Introductionmentioning
confidence: 99%
“…Integration of coarse spatial resolution microwave data with an optical/thermal infrared retrieval using a downscaling factor is the most extensively used satellite-based approach (Moran et al, 2004;Mobasheri, 2016;Gao et al, 2017;Amazirh et al, 2018) Serrano et al, 2004;Amazirh et al, 2018). TVDI is frequently utilized due to its great precision and ease in monitoring soil moisture (Younis and Iqbal, 2015;Paddies, 2016;Peng et al, 2020;Kazemzadeh et al, 2021). TVDI is an optical/thermal remote sensing metric related to soil moisture fluctuation.…”
Section: Introductionmentioning
confidence: 99%
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