The accretion rate of supercooled water droplets onto the hailstone depends on the relative velocities between these water droplets and the hailstone itself.
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It was thought that the seeding would cause supercooled water in the outer rainbands to freeze, causing the inner eyewall to collapse and thus reducing the winds.
Researchers conducted the first reported study of the freezing process of levitated single submicrometre-sized droplets in air using optical trapping techniques, including supercooled water droplets at 228 K.
This derivation of the Gibbs–Thomson equation appears on pages 417–418 of: James E. McDonald (December 1953) "Homogeneous nucleation of supercooled water drops", Journal of Meteorology, 10 : 416–433.
And where supercooled water, which remains liquid at lower depths due to the high pressure, is squeezed up valley walls into areas where the pressure drops, it can freeze very quickly.
Sólo danos un día para encontrar quien tramó estocordis cordis