2019
DOI: 10.1109/tap.2019.2913785
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Use and Accuracy of Numerical Weather Predictions to Support EM Wave Propagation Experiments

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Cited by 13 publications
(13 citation statements)
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“…Radiometric measurements with high time resolution (∼ 4 s) show rapid fluctuations for lower values of ICLWC that ERA-5 or RAOBS data with much coarser time resolution do not capture. When compared to RAOBS and ERA-5, radiometric cloud attenuation measurements give a higher percentage occurrence of lower cloud attenuation [9]. In this regard it may be mentioned that current radiometric measurements yield low ICLWC values (less than 0.5 mm) for 91 % of time compared to 85% for RAOBS and 80% for ERA-5.…”
Section: Acl(f)=aclwc(f)iclwcmentioning
confidence: 88%
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“…Radiometric measurements with high time resolution (∼ 4 s) show rapid fluctuations for lower values of ICLWC that ERA-5 or RAOBS data with much coarser time resolution do not capture. When compared to RAOBS and ERA-5, radiometric cloud attenuation measurements give a higher percentage occurrence of lower cloud attenuation [9]. In this regard it may be mentioned that current radiometric measurements yield low ICLWC values (less than 0.5 mm) for 91 % of time compared to 85% for RAOBS and 80% for ERA-5.…”
Section: Acl(f)=aclwc(f)iclwcmentioning
confidence: 88%
“…The processing of satellite beacon signals enables the retrieval of the excess attenuation due to rain. The total attenuation necessitates an evaluation of the attenuation due to gases and clouds, called non-rainy attenuation [9], [10]. The latter can be obtained from a co-located radiometer with the same elevation and azimuth as the beacon receiver antenna.…”
Section: Introductionmentioning
confidence: 99%
“…Characteristic integrated values for wind speed (WS) and turbulence strength (C N 2 ), derived from the European Center for Medium Weather Forecast (ECMWF) database (Molteni et al, 1996), can be considered as proxy parameters for the presence of turbulent eddies in the lower portions of the atmosphere, which affect the accuracy of the TDCS calibrations (Lasagni Manghi et al, 2019). Both values of wind speed and turbulence strength were provided by UCL (Quibus et al, 2019) and were derived by averaging over time the local vertical profiles from the ECMWF data set that fell within the tracking pass interval. The obtained vertical profiles were then spatially averaged from ground level to a height of 1 km above the surface.…”
Section: Testbed Summary and Data Availabilitymentioning
confidence: 99%
“…Additionally, the NAS can be employed to set the clear sky level (recover the attenuation in non-rainy conditions) in place of the radiometer [19].…”
Section: Numerical Atmospheric Simulatormentioning
confidence: 99%