1995
DOI: 10.1016/0034-4257(94)00074-w
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Status of microwave soil moisture measurements with remote sensing

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Cited by 299 publications
(126 citation statements)
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“…The very nature of SAR imaging (and all imaging) is that the surface or target under study can be described only at that one particular instance when the image was acquired. While many change detection techniques have been proposed and utilised for the analysis of images acquired by optical sensors, less attention has been devoted to change detection using SAR data [134] due to its inherent complexity in terms of processing and in the development of effective data analysis techniques to minimise speckle [135,136].…”
Section: Soil Moisture Retrieval Using a Change Detection Approachmentioning
confidence: 99%
“…The very nature of SAR imaging (and all imaging) is that the surface or target under study can be described only at that one particular instance when the image was acquired. While many change detection techniques have been proposed and utilised for the analysis of images acquired by optical sensors, less attention has been devoted to change detection using SAR data [134] due to its inherent complexity in terms of processing and in the development of effective data analysis techniques to minimise speckle [135,136].…”
Section: Soil Moisture Retrieval Using a Change Detection Approachmentioning
confidence: 99%
“…Conventional field measurement techniques have serious limitations in their ability to appropriately estimate the spatial distribution of soil moisture, particularly over large areas that are characterized by soil surface heterogeneity [3]. Most hydrological models require soil moisture information and use point measurements or spatial distributed soil moisture values derived from physically-based land surface models [1,2,[4][5][6]. Presently, however, spatial distributions of high resolution soil moisture estimates are being used as input to hydrological models to predict the runoff [2,7,8].…”
Section: Introductionmentioning
confidence: 99%
“…Thus, the radar observation depth is a function of the soil moisture and it is greater for dryer soil than for moist soil. As well as the soil moisture, the remote sensing observation depth is also depending on free space wavelength, incidence angle, wave polarization, surface roughness and vegetation cover [36][37][38]. The radar penetration depth δ p , which has been introduced by Ulaby et al [39], is a function of the radar frequency system and soil moisture (soil dielectric constant).…”
Section: Theorymentioning
confidence: 99%