But Dumont and her colleagues have found that, since 2009, there has been a darkening that can not be explained by
larger snow grain size alone.
Not exact matches
Third, it can explicitly account for the
large displacements and rearrangement of the
snow grains during deformation.
At the same time, as the
snow melts and refreezes, the
grains of
snow get
larger.
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.
Scientists have generally attributed that darkening to
larger, slightly less white
snow grains caused by warmer temperatures.
«When
snow first falls,
snow grains are quite small, and as snowpack ages, and particularly for warmer snowpack, you get consolidation of those
grains into
larger clumps,» said Sarah Doherty, a researcher at the University of Washington who co-authored the paper.
The relatively
large temperature response is related to positive feedbacks which enhance the initial impact of changed
snow grain size.
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.
The relatively
large temperature response is related to positive feedbacks which enhance the initial impact of changed
snow grain size.