Since the reduction of
albedo by grain growth is confined to the near infrared, it is mostly invisible to our eyes.
Not exact matches
Simulating the variation of the ice sheet's
albedo using a regional climate model — Modèle Atmosphérique Régionale (MAR), which some members of the team helped develop — indicated that increasing temperatures and melting accompanied
by snow
grain growth and greater bare ice exposure account for about half the decline, the scientists report.
When the snow
grains were assumed nonspherical, snow
albedo was increased slightly, typically
by 2 - 3 percentage units.
snow
albedo) was modified in the NorESM climate model,
by replacing an approach based on spherical snow
grains with an approach assuming nonspherical snow
grains.
The more soot, the more darkening, but as little as a few parts per billion
by weight reduces the
albedo of pure snow (that is, collections of
grains of ice)
by a few per cent in the visible part of the spectrum.
For pure snow,
grain growth from new snow (
grains around 0.1 millimeter in radius) to old melting snow (radius around 1 millimeter) can reduce broadband
albedo by around 10 %.