Snow grains become rounded.
The first rainfall of the season causes metamorphosis of the snow grains, whereby the snow becomes wet and individual
snow grains become larger, which makes the snow less reflective.
Not exact matches
Two properties dominate reflectivity in dry
snow — the size of
snow grains, which
become larger and more absorbent as they melt, and the presence of dark impurities that absorb the sun's energy, predominantly black carbon and mineral dust, which also cause the
snow to melt faster.
In melting
snow,
grains become further rounded and clump into clusters.