2020
DOI: 10.1002/essoar.10504288.1
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Wind Tunnel Validation of a Particle Tracking Model to Evaluate the Wind-Induced Bias of Precipitation Measurements.

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Cited by 5 publications
(5 citation statements)
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“…The Lagrangian Particle Tracking (LPT) model used by [9] for solid precipitation was modified by [24] to introduce drag coefficient equations suitable for liquid precipitation. These were derived for various ranges of the particle Reynolds number among those proposed in the literature by [7], and formulated starting from data published by [25,26].…”
Section: Methodsmentioning
confidence: 99%
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“…The Lagrangian Particle Tracking (LPT) model used by [9] for solid precipitation was modified by [24] to introduce drag coefficient equations suitable for liquid precipitation. These were derived for various ranges of the particle Reynolds number among those proposed in the literature by [7], and formulated starting from data published by [25,26].…”
Section: Methodsmentioning
confidence: 99%
“…Water drops are assumed to be spherical, with the associated equivalent diameter 𝑑, while the density of liquid water was set as equal to 1000 kg m −3 at the air temperature of 20 °C. This model was validated by means of a dedicated wind tunnel campaign in [24].…”
Section: Methodsmentioning
confidence: 99%
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“…The gauge body, immersed in a wind field, behaves like a bluff‐body obstacle in the free flow, and produces strong velocity gradients, upwards or downwards components and turbulence close to the gauge (Cauteruccio et al, 2020). The hydrometeors trajectories are diverted by the velocity field around the instrument (Cauteruccio et al, 2021a; Cauteruccio et al, 2021b; Cauteruccio et al, 2021c; Colli et al, 2020; Folland, 1988; Jevons, 1861; NeĆĄpor & Sevruk, 1999) and, depending on the gauge shape and wind speed, the number of hydrometeors that cross the sensing volume is affected, leading to an over‐ or under‐estimation of the precipitation intensity. The exposure effect therefore introduces an error, common to all precipitation gauges, that is simply due to the presence of the instrument itself (invasive measurement) and varies with the gauge shape, wind speed and direction, and the PSD.…”
Section: Influence Of Parametersmentioning
confidence: 99%
“…The gauge body, immersed in a wind field, behaves like a bluff-body obstacle to the undisturbed airflow, producing strong velocity gradients, vertical components, and the development of turbulence close to the gauge surface, see, e.g., [ 4 , 5 ]. The hydrometeor trajectories are diverted by the velocity field around the instrument [ 6 ] depending on their diameter, the gauge shape, wind speed, and wind direction. The induced change in the number of hydrometeors that cross the sensing volume/collecting area of the gauge (for NCGs and CGs, respectively) can lead, in windy conditions, to an over or under estimation of the precipitation amount and intensity (see, e.g., [ 7 ]).…”
Section: Introductionmentioning
confidence: 99%