
Wind farms in cold climates face a unique challenge: icing. When temperatures drop below freezing, moisture in the air can freeze onto turbine blades, altering their shape and weight. This reduces aerodynamic efficiency and can also lead to mechanical issues and safety risks. Accurate icing calculations are essential for designing turbines that can operate in harsh conditions and for planning maintenance to minimise downtime.
Vortex ICING allows quantification of the meteorological icing phase, during which atmospheric conditions are favourable for ice accretion. During this phase, ice accumulates on infrastructures, such as sensors and turbine blades.
First, Vortex runs a 10-year, hourly time-series simulation with the WRF model at 3-km horizontal resolution to identify cold periods with potential icing conditions using a temperature threshold.
Once these periods are detected, a second simulation is run at higher spatial resolution (1 km), focused on the potential icing days. This simulation uses a microphysics scheme that better represents cloud properties relevant for icing, especially the qcloud variable (Thompson scheme), which allows to identify and filter better the most humid days. From this high-resolution simulation, we determine the candidate icing periods, which are cold and humid days.
For this subset of days, we run a FARM simulation at 100-m resolution covering the domain defined by the user. This FARM provides a more accurate wind-speed estimation for the Makkonen icing model, as well as qcloud values needed to compute the icing accretion rate (dm/dt).
The model assumes that icing occurs when supercooled cloud droplets impact a cold surface and freeze. Three factors control the process:
In simplified form, the icing rate is expressed as:
dm/dt = α · β · ρw · M · LWC
In practice, colder temperatures increase sticking efficiency, stronger winds increase droplet impacts, and higher cloud-water content provides more available liquid. This makes the Makkonen model both physically consistent and practical, requiring only wind speed and cloud-liquid content—exactly the variables produced by the Vortex high-resolution simulations.
The outputs of Vortex Icing are two types: map layers for the full domain, and time series and reports for specific points. All heights are available between 50 and 300 m.
Map layers can be delivered as ESRI grids, Google Earth KMZ files, or WRG files.
YYYYMMDD HHMM dmdt(g/h) T100(C) Tref(C) Mref(m/s) Dref(deg) RHref(%) 20201126 2300 - - -0.1 6.3 185 98.4 20201127 0000 - - 0.1 7.1 195 98.4 20201127 0100 16.6 -0.2 0.2 9.4 206 98.3 20201127 0200 12.2 -0.4 0.2 10.5 211 98.3 20201127 0300 19.4 -0.2 0.1 10.9 213 98.5 20201127 0400 40.3 0.1 0.1 10.9 214 98.8 20201127 0500 64.5 -0.1 0.1 10.4 218 99.5 20201127 0600 76.3 -0.1 -0.1 9.6 221 100.0 20201127 0700 72.6 -0.2 -0.1 8.6 223 100.0 20201127 0800 53.8 -0.3 -0.1 7.9 226 100.0 20201127 0900 43.9 -0.3 -0.2 7.5 232 100.0 20201127 1000 38.3 -0.6 -0.6 7.2 238 99.4 20201127 1100 17.8 -1.0 -0.8 7.0 237 97.5 20201127 1200 - - -1.1 7.0 234 96.7 20201127 1300 - - -1.4 7.0 232 96.4
The report summarises icing statistics at each turbine location:
Accurate icing modeling is key to minimizing downtime and maximizing performance in cold climates. With Vortex ICING, you get the high-resolution data needed to turn weather risks into manageable project insights.
Modeled wind resource data for the wind industry.
At any site around the world. Onshore and offshore.