2010
DOI: 10.1007/s00704-010-0316-5
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Identifying precipitating clouds in Greece using multispectral infrared Meteosat Second Generation satellite data

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Cited by 38 publications
(53 citation statements)
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“…Brightness temperature ΤIR10.8 is an indication of the vertical extent of the cloud because, in general, brightness temperature of the system depends on the cloud-top height [2,16,17,18,19,20].…”
Section: A Spectral Parametersmentioning
confidence: 99%
“…Brightness temperature ΤIR10.8 is an indication of the vertical extent of the cloud because, in general, brightness temperature of the system depends on the cloud-top height [2,16,17,18,19,20].…”
Section: A Spectral Parametersmentioning
confidence: 99%
“…Techniques for rain area delineation relying on different spectral parameters have already been developed (e.g., Thies et al 2008b, c;Feidas and Giannakos 2010). Since the objective of the present study is to explicitly evaluate the potential of classifying rainy clouds as convective and stratiform based on spectral properties of cloud tops, only precipitating gauge data are considered.…”
Section: Data Preprocessingmentioning
confidence: 99%
“…In order to develop convective/stratiform rain type classification techniques, this study has adopted the procedure proposed by Feidas and Giannakos (2010) for the discrimination between precipitating and nonprecipitating clouds over Greece. In our case, two different methods were used to develop schemes for discriminating between convective and stratiform rainy clouds.…”
Section: Techniques' Developmentmentioning
confidence: 99%
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