Sliding prior to and during early freezing dominates the asymmetry of the frozen droplet, producing a tilted ice cusp whose angle depends on inclination and wettability.
& Zhang, X.2022 A new freezing model of sessile droplets considering ice fraction and ice distribution after recalescence
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Asymmetric freezing of a sliding droplet on an inclined surface
Sliding prior to and during early freezing dominates the asymmetry of the frozen droplet, producing a tilted ice cusp whose angle depends on inclination and wettability.