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Assessment and Impact of Soil Moisture Index in Agricultural Drought Estimation Using Remote Sensing and GIS Techniques

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dc.contributor.author Saha, Arnab
dc.contributor.author Patil, Manti
dc.contributor.author Goyal, V. C.
dc.contributor.author Rathore, D. S.
dc.date.accessioned 2020-07-02T06:20:16Z
dc.date.available 2020-07-02T06:20:16Z
dc.date.issued 2018
dc.identifier.citation 3rd International Electronic Conference on Water Sciences, 15–30 November 2018 en_US
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/4436
dc.description.abstract Soil moisture takes an important part involving climate, vegetation and drought. This paper explains how to calculate the soil moisture index and the role of soil moisture. The objective of this study is to assess the moisture content in soil and soil moisture mapping by using remote sensing data in the selected study area. We applied the remote sensing technique which relies on the use of the soil moisture index (SMI) which uses the data obtained from satellite sensors in its algorithm. The relationship between land surface temperature (LST) and the normalized difference vegetation index (NDVI) are based on experimental parameterization for the soil moisture index. Multispectral satellite data (visible, red and near-infrared (NIR) and thermal infrared sensor (TIRS) bands) were utilized for assessment of LST and to make vegetation indices map. Geographic Information System (GIS) and image processing software were utilized to determine the LST and NDVI. NDVI and LST are considered as essential data to obtain SMI calculation. The statistical regression analysis of NDVI and LST were shown in standardized regression coefficient. NDVI values are within range −1 to 1 where negative values present loss of vegetation or contaminated vegetation, whereas positive values explain healthy and dense vegetation. LST values are the surface temperature in °C. SMI is categorized into classes from no drought to extreme drought to quantitatively assess drought. The final result is obtainable with the values range from 0 to 1, where values near 1 are the regions with a low amount of vegetation and surface temperature and present a higher level of soil moisture. The values near 0 are the areas with a high amount of vegetation and surface temperature and present the low level of soil moisture. The results indicate that this method can be efficiently applied to estimate soil moisture from multi-temporal Landsat images, which is valuable for monitoring agricultural drought and flood disaster assessment. en_US
dc.language.iso en en_US
dc.publisher MDPI en_US
dc.subject Soil moisture index (SMI) en_US
dc.subject LST en_US
dc.subject NDVI en_US
dc.subject Drought en_US
dc.title Assessment and Impact of Soil Moisture Index in Agricultural Drought Estimation Using Remote Sensing and GIS Techniques en_US
dc.type Article en_US


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