2007
DOI: 10.1029/2007gl031715
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A new technique for estimating outgoing longwave radiation using infrared window and water vapor radiances from Kalpana very high resolution radiometer

Abstract: [1] A new technique for estimating the outgoing longwave radiation (OLR) from the radiances observations in the infrared window (WIN; 10.5 -12.5 mm) and water vapor (WV; 5.7-7.1 mm) channels onboard the geostationary operational Indian National Satellite (INSAT) Kalpana has been developed. The OLR is estimated from the WIN and WV radiances via genetic algorithm (GA). The transfer functions that relate OLR and narrowband radiances (WIN and WV) were developed using radiative transfer model. It is shown that incl… Show more

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Cited by 15 publications
(11 citation statements)
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References 19 publications
(27 reference statements)
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“…For the two following examples, we use model results from simulations with the Weather Research and Forecasting (WRF) model (Skamarock et al, 2005). These simulations use the Morrison microphysics scheme (Morrison et al, 2005(Morrison et al, , 2009 and the Rapid Radiative Transfer Model (RRTMG) shortwave and longwave radiation scheme (Iacono et al, 2008).…”
Section: Advantages Of the Implementation In Pythonmentioning
confidence: 99%
“…For the two following examples, we use model results from simulations with the Weather Research and Forecasting (WRF) model (Skamarock et al, 2005). These simulations use the Morrison microphysics scheme (Morrison et al, 2005(Morrison et al, , 2009 and the Rapid Radiative Transfer Model (RRTMG) shortwave and longwave radiation scheme (Iacono et al, 2008).…”
Section: Advantages Of the Implementation In Pythonmentioning
confidence: 99%
“…OLR retrievals also have the benefit that they do not depend on other aspects of a complicated radiative transfer model, which require, amongst other assumptions, that pixels are assigned as either cloud or cloud-free for the radiative retrieval of several optical (effective radius and optical depth) and thermal (cloud top temperature and height) cloud properties (McGarragh et al, 2018). For the satellite data, we use an empirical conversion derived in Singh et al (2007) to convert the radiances L from two channels in the GOES-13 measurements, the water vapour channel (WV, 5.8 to 7.30 µm) and a channel in the infrared window (WIN, 10.2 to 11.2 µm), to OLR. Singh et al (2007) report an uncertainty from these conversions within 2.5 W m −2…”
Section: Time Resolution Requirements For Cloud Trackingmentioning
confidence: 99%
“…For the satellite data, we use an empirical conversion derived in Singh et al (2007) to convert the radiances L from two channels in the GOES-13 measurements, the water vapour channel (WV, 5.8 to 7.30 µm) and a channel in the infrared window (WIN, 10.2 to 11.2 µm), to OLR. Singh et al (2007) report an uncertainty from these conversions within 2.5 W m −2…”
Section: Time Resolution Requirements For Cloud Trackingmentioning
confidence: 99%
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“…Based on radiative transfer simulations for a set of diverse atmospheric profiles, the accuracy of the Meteosat OLR product is shown to be ∼3 W m −2 [ Schmetz and Liu , 1988]. Singh et al [2007] also found that the accuracy of OLR products derived for Kalpana satellite using a narrowband‐to‐broadband conversion method is ∼2.5 W m −2 . The validation of the OLR product derived from the GOES with broadband OLR observations from the Clouds and the Earth's Radiant Energy System (CERES) onboard polar orbiting satellites Tropical Rainfall Measuring Mission (TRMM) and EOS‐Terra reveal that the accuracy of the narrowband‐to‐broadband flux computation is ∼7 W m −2 on a daily time scale [ Ba et al , 2003].…”
Section: Datamentioning
confidence: 99%