2000
DOI: 10.1098/rsta.2000.0690
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Models for the growth of rime, glaze, icicles and wet snow on structures

Abstract: Ice accretion on structures is discussed with an emphasis on estimating structural design iceloads and solving operational icing problems. Basic principles of modelling of icing caused by freezing precipitation, cloud droplets and wet snow, as well as simulation of icicle growth, are presented. Theoretical models of atmospheric ice accretion are critically reviewed, particularly with respect to the simulation of the relevant physical processes. The reasons for the difficulties in simulating some icing phenomen… Show more

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Cited by 288 publications
(251 citation statements)
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“…Radiation is simulated using the RRTM longwave radiation scheme and the Dudhia shortwave radiation scheme. (2000): droplet flow around a cylinder (taken from Makkonen, 2000). …”
Section: Forecasts Of Icingmentioning
confidence: 99%
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“…Radiation is simulated using the RRTM longwave radiation scheme and the Dudhia shortwave radiation scheme. (2000): droplet flow around a cylinder (taken from Makkonen, 2000). …”
Section: Forecasts Of Icingmentioning
confidence: 99%
“…In the current study, icing simulations are based on results of the weather research and forecasting (WRF) model coupled to an icing algorithm (Makkonen, 2000). WRF is a state-of-the-art non-hydrostatic numerical model for high resolution weather forecasts (Skamarock et al, 2008).…”
Section: Forecasts Of Icingmentioning
confidence: 99%
See 1 more Smart Citation
“…where M is the mass of ice, t is the time, α 1 ,α 2 and α 3 are efficiency coefficients, W is liquid water content, v is wind speed and A is the cross-sectional area of the cylinder on which the ice accumulation is calculated (Makkonen, 2000). The 20 efficiency coefficients take into account aspects of the object where the ice is accumulated, such as the possibility for water adhering to the surface.…”
mentioning
confidence: 99%
“…The 20 efficiency coefficients take into account aspects of the object where the ice is accumulated, such as the possibility for water adhering to the surface. A detailed description of the coefficients is found in Makkonen (2000). Meteorological inputs needed for the ice calculations are temperature, wind speed, liquid water content and median volume droplet size.…”
mentioning
confidence: 99%