2014
DOI: 10.1002/qj.2298
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Doppler radar radial wind assimilation using an hourly cycling 3D‐Var with a 1.5 km resolution version of the Met Office Unified Model for nowcasting

Abstract: This article describes the development and trials at the Met Office of the assimilation of radar Doppler radial winds in a pre‐operational framework. It uses a high‐resolution 1.5 km convective‐scale version of the Unified Model for nowcasting, on a small domain covering southern England and Wales. The assimilation was performed using a version of the Met Office 3D‐variational data assimilation system at 1.5 km resolution. The Doppler radial wind observations were provided by the original four Dopplerized C‐ba… Show more

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Cited by 63 publications
(87 citation statements)
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“…Therefore, experiments were undertaken for a domain covering southern England and Wales with hourly‐cycling 3D‐Var (Ballard et al, , ) and then with 4D‐Var (Golding et al , ; Sun et al , ; Ballard et al , ). This system was extended to allow assimilation of radar Doppler radial winds (Simonin et al , ), which were then introduced operationally in the UKV model in 2011. Work is underway to develop direct assimilation of radar reflectivity (Hawkness‐Smith and Ballard, ) and ceilometer backscatter as well as radar refractivity (Nicol et al , ).…”
Section: Data Assimilation For Convection‐permitting Modelsmentioning
confidence: 99%
“…Therefore, experiments were undertaken for a domain covering southern England and Wales with hourly‐cycling 3D‐Var (Ballard et al, , ) and then with 4D‐Var (Golding et al , ; Sun et al , ; Ballard et al , ). This system was extended to allow assimilation of radar Doppler radial winds (Simonin et al , ), which were then introduced operationally in the UKV model in 2011. Work is underway to develop direct assimilation of radar reflectivity (Hawkness‐Smith and Ballard, ) and ceilometer backscatter as well as radar refractivity (Nicol et al , ).…”
Section: Data Assimilation For Convection‐permitting Modelsmentioning
confidence: 99%
“…For the BoM's developmental ACCESS-City LAMs, only echoes classed as precipitation are assumed to be qualified for assimilation. The observations undergo extensive processing after ingestion in the assimilation system [the details of the quality control options are like those in Simonin et al (2014)], including observation-minusbackground checks, removal of isolated pixels, and comparison with neighbors, before spatial averaging to reduce data density. This means that classification is not the only mechanism for removing unreliable velocity observations.…”
Section: Application To Doppler Radar Data Assimilationmentioning
confidence: 99%
“…This means that classification is not the only mechanism for removing unreliable velocity observations. Note that for radial velocity, misclassification at long range may not be a large problem because observations far from the radar are not assimilated due to increasing error contributions (Fabry 2010;Simonin et al 2014). Currently, a range limit of 100 km is applied for assimilated observations.…”
Section: Application To Doppler Radar Data Assimilationmentioning
confidence: 99%
“…Doppler capability also allows winds to be estimated in precipitation with similar spatial and temporal resolution, enabling the detection of hazards such as wind shear. The assimilation of these observations has been shown to improve rain and wind significantly in NWP‐based nowcasts (Simonin et al , ).…”
Section: Protecting Lives and Livelihoodsmentioning
confidence: 99%