1987
DOI: 10.1175/1520-0493(1987)115<1773:tnocpe>2.0.co;2
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The NESDIS Operational Convective Precipitation- Estimation Technique

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Cited by 144 publications
(63 citation statements)
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“…At NOAA, the H-E estimates have been used since the late 1970's. At first it was used for the Interactive Flash Flood Analyzer [10], before it was used as fully automated Auto-Estimator Vicente, Scofield and Menzel [11]. The current-generation operational algorithm at NESDIS is the Hydro-Estimator (H-E) which has been used since 2002 [12].…”
Section: Satellite Datamentioning
confidence: 99%
“…At NOAA, the H-E estimates have been used since the late 1970's. At first it was used for the Interactive Flash Flood Analyzer [10], before it was used as fully automated Auto-Estimator Vicente, Scofield and Menzel [11]. The current-generation operational algorithm at NESDIS is the Hydro-Estimator (H-E) which has been used since 2002 [12].…”
Section: Satellite Datamentioning
confidence: 99%
“…Ba and Gruber (2001) used the GOES visible (0.65 µm), near-infrared (3.9 µm), water vapour (6.7 µm) and window channels (10.7 and 12.0 µm) to estimate rainfall rate, distinguishing raining from non-raining clouds by taking into account the cloud top temperature, the effective radius of cloud particles and the temperature gradient. Moreover, in an attempt to give more reliable values of rain rates, Ba and Gruber (2001) used the moisture factor correction developed by Scofield (1987) and modified by Vicente et al (1998). Other authors used artificial neural networks to derive precipitation estimates using satellite IR images (Hsu et al, 1997;Behrangi et al, 2009;Capacci and Porcù, 2009).…”
Section: E Ricciardelli Et Al: a Statistical Approach For Rain Intementioning
confidence: 99%
“…Griffith et al (1978) present the Griffith-Woodley technique based on the study of the life cycle of clouds. The hydroestimator (HE) technique (Vicente et al 1998(Vicente et al , 2002) is based on the methodology developed by Scofield (1987). To compute rainfall rates, it uses a nonlinear power-law relationship between cloud-top temperature and radar-derived rainfall-rate estimates, a gradient and growth-rate mask, and a humidity mask.…”
Section: Introductionmentioning
confidence: 99%
“…RESAT is based on both pixel and cloud-patch properties. Griffith et al (1978), Scofield (1987), Feidas and Cartalis (2001), Mathon and Laurent (2001), and Schumacher and Johnson (2005) point out the importance of the relationship between the life cycle of the MCS and the rainfall it produces. In spite of this, in some cases only qualitative relationships are given and in others cases some problems arise due to the limitations of cloud-patch-based methods.…”
Section: Introductionmentioning
confidence: 99%
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