Meteorological icing: Difference between revisions
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The meteorological icing is defined as the period during which the meteorological conditions (temperature, wind speed, liquid water content, droplet distribution) allow for ice accretion. | The meteorological icing is defined as the period during which the meteorological conditions (temperature, wind speed, liquid water content, droplet distribution) allow for ice accretion. <ref>Ville Lehtomäki, Andreas Krenn, Pieter Jan Jordaens, Charles Godreau, Neil Davis, Zouhair Khadiri-Yazami, Rolv Erlend Bredesen, Göran Ronsten, Helena Wickman, Saskia Bourgeois, and Till Beckford, IEA Wind TCP Task 19 – Available Technologies for Wind Energy in Cold Climates, 2nd Edition, IEA Wind Task 19, 2018.</ref> | ||
== References == | |||
Latest revision as of 11:39, 11 February 2022
The meteorological icing is defined as the period during which the meteorological conditions (temperature, wind speed, liquid water content, droplet distribution) allow for ice accretion. [1]
References
- ↑ Ville Lehtomäki, Andreas Krenn, Pieter Jan Jordaens, Charles Godreau, Neil Davis, Zouhair Khadiri-Yazami, Rolv Erlend Bredesen, Göran Ronsten, Helena Wickman, Saskia Bourgeois, and Till Beckford, IEA Wind TCP Task 19 – Available Technologies for Wind Energy in Cold Climates, 2nd Edition, IEA Wind Task 19, 2018.