2018
DOI: 10.3390/rs10091453
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Mesoscale Resolution Radar Data Assimilation Experiments with the Harmonie Model

Abstract: This study presents a pre-processing approach adopted for the radar reflectivity data assimilation and results of simulations with the Harmonie numerical weather prediction model. The proposed method creates a 3D regular grid in which a horizontal size of meshes coincides with the horizontal model resolution. This minimizes the representative error associated with the discrepancy between resolutions of informational sources. After such preprocessing, horizontal structure functions and their gradients for radar… Show more

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Cited by 6 publications
(3 citation statements)
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“…New sources of observation data such as LIDAR and floating LIDAR have the potential to provide wind data at multiple heights for less cost than traditional met masts (Gottschall, Gribben, Stein, & Würth, ), while data assimilation of radar reflectivities has been shown to improve the representation of clouds and precipitation in NWP (Ivanov, Michaelides, & Ruban, ).…”
Section: The Future Of Forecasting Renewable Energymentioning
confidence: 99%
“…New sources of observation data such as LIDAR and floating LIDAR have the potential to provide wind data at multiple heights for less cost than traditional met masts (Gottschall, Gribben, Stein, & Würth, ), while data assimilation of radar reflectivities has been shown to improve the representation of clouds and precipitation in NWP (Ivanov, Michaelides, & Ruban, ).…”
Section: The Future Of Forecasting Renewable Energymentioning
confidence: 99%
“…Ivanov et al [9] present a pre-processing approach adopted for the radar reflectivity data assimilation and results of simulations with the Harmonie numerical weather prediction model. The proposed method creates a 3-D regular grid in which a horizontal size of meshes coincides with the horizontal model resolution.…”
Section: Overview Of Contributionsmentioning
confidence: 99%
“…Numerous operational nowcasting systems use the relationship between static radar reflectivity (Z) and the rain rate (R), such as the commonly used Marshall-Palmer [18] formula of Z = 200 R 1.6 , to convert radar echo into rainfall estimates. Radar-and gauge-based rainfall estimates are typically consistent, particularly when the rainfall intensity is high [19][20][21][22][23][24][25]. Researchers have studied the QPE of tropical cyclones.…”
Section: Introductionmentioning
confidence: 99%