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Radar Vegetation Index as an Alternative to NDVI for Monitoring of Soyabean and Cotton

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The study explores the possibility of Radar Vegetation Index (RVI) for vegetation monitoring in Cotton and Soya bean fields as an alternative to monitoring with Normalized Difference Vegetation Index (NDVI). The RVI is the measure randomness of scattering has been proposed as a method for monitoring the level of vegetation growth, particularly when time series of data are available. The SAR can penetrate the clouds thus it has the potential to monitor the crop growth in all the seasons. This point is very important in the context of Indian subcontinent since monsoon clouds hampering the monitoring of crops in such season. The present study carried out in Vidharba region of Maharashtra, India using four Radarsat-2 data sets acquired in the monsoon season of 2011 (ie: 13thJuly 2011, 06thAugust 2011, 30 August 2011, 23rdSeptember 2011). The derived RVI was compared with the MODIS NDVI product of same date. The research shows some significant improvements in the RVI technique than NDVI in some context. The RVI is linearly increasing as crop grows unlike the NDVI becomes saturated after level of growth in the crop. The Cultivation started in the first week of July 2011, the NDVI becomes saturated mostly in second week of August, 2011 however RVI shows further increase in 30th August 2011 with the growth in the vegetation. These particular findings attributed to the fact that maximum randomness of scattering in microwave signal occurs where plant spread fully whereas peak greenness (NDVI) occurs before that. The present study found that RVI can be utilised in place of NDVI for vegetation monitoring thus monitoring of crops is possible even in the monsoon season of India. This method can be better used with RISAT descending mode since its acquiring image on optimum incident angle of around 360 look angle thus it is highly suitable for vegetation monitoring. The Radar Vegetation Index can also have the prospect of using in soil moisture models in vegetated fields where NDVI is a critical one (Kim and J. Van Zyl ., 2009). The result of this study can be effectively used for monitoring soyabean and cotton and also can be used as a vegetation mask for soil moisture monitoring. The further study is required to derive biophysical parameters from RVI and application of RVI in soil moisture estimation in vegetated fields
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... approach, which is commonly employed in research using optical image processing (De Luca et al., 2022). RVI, which has a value between 0 and 1 were used to assess the randomness of scattering in SAR (Kumar et al., 2013). Sentinel-1, being equipped with dual polarization capabilities, offers both VH and VV polarizations, as discussed in the studies conducted by Charbonneau et al. (2005) and Kim and Van Zyl (2009). ...
... The range of the RVI typically spans from 0 to 1. According to (Ratha et al., 2019) the RVI values for vegetation areas range from 0.3 to 0.6 and For a smooth bare surface, the RVI is near zero and it increases as the crop grows as volume scattering (Kumar et al., 2013). This study's RVI value range was around 0.309-0.360 ...
... These models enable the monitoring of plant phenological changes during the growing season. Also, according to Kumar et al. (2013), RVI is highly suitable than NDVI and can be used for monitoring crops throughout the crop cycle. However, RVI is impacted by vegetation and soil moisture, respectively, and these indices are also affected by long-term weather conditions (S. W. Kim et al., 2020). ...
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... However, NDVI is limited by its dependence on optical data. In contrast, the Radar Vegetation Index (RVI), which is calculated from radar data, is a powerful tool for monitoring and analyzing temporal variations in vegetation and offers a reliable alternative that allows for consistent, all-weather monitoring (Kumar et al., 2013). While other indices like the Dual-Polarization RVI (DpRVI) exist, RVI's simpler formulation and effectiveness in time series agricultural monitoring support its use in this study (Salsabila et al., 2021;Szigarski et al., 2018). ...
... The RVI is a widely recognized microwave-based vegetation index utilized for crop growth monitoring. For dual-pol SAR data, RVI is derived using the following formula (Kumar et al., 2013) Here, the radar backscattering coefficient (σ 0 ) indicates the intensity of the signal scattered by the surface. It is also known as radar cross-section per unit area (Kaplan et al., 2021). ...
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... From these images, backscattering coefficients were extracted for σ 0 VV (vertical transmit and receive polarization), σ 0 VH (vertical transmit and horizontal receive polarization), σ 0 VV + σ 0 VH, and the Radar Vegetation Index (RVI). The use of RVI (Equation 1) is the replacement for NDVI which is crucial for vegetation health monitoring (Kumar et al., 2013). These backscattering values are sensitive to soil moisture and vegetation characteristics, making them suitable indicators for modeling soil moisture levels (Wagner et al., 2007). ...
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... Where FVC RVI represents the community structure and is computed by means of the pixel dichotomy model. Given the correlation between RVI and NDVI (Kim et al. 2015;Kumar, Rao, and Sharma 2013), as well as the intermittent nature of NDVI acquisitions, the combination of the more temporally continuous RVI and the pixel dichotomy model (Gao et al. 2020) is employed to obtain FVC RVI : ...
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... Otherwise, RVI is a measurement of volumetric scattering, whereas NDVI is a measure of greenness due to the presence of chlorophyll. The plant attains maximum greenness before it reaches volumetric maturity (Kumar et al. 2013). ...
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Several successful algorithms have been developed to estimate soil moisture of bare surfaces. We previously reported a new algorithm using the tilted Bragg approximation. However, these algorithms are only applicable to bare surfaces. When vegetation is present, soil moisture is typically underestimated by bare surface algorithms. In order to derive soil moisture under vegetation, we have to understand the complex scattering process due to vegetation. Our main interest is to retrieve the global soil moisture information using Hydros L-band polarimetric radar data. The Hydros mission will provide the first global view of land soil moisture using L-band radar and radiometer. The unique characteristics of the Hydros data are the availability of the low resolution soil moisture information from radiometer data and the continuous time series radar data collected at the same incidence angle. In this paper, we will examine a potential inversion algorithm to retrieve soil moisture under vegetation canopies using Hydros L-band polarimetric radar data
Use of Dual Polarization and Multi-Incidence SAR for soil permeability mapping
  • F Charbonneau
  • M Trudel
  • R Fernandes
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