Mishchenko, M.I., and K. Sassen, 1998: Depolarization of lidar returns
by small ice crystals: An application to contrails.
Not exact matches
When the snow gets packed down
by subsequent layers, the space between the
crystals is eventually sealed off, trapping a
small sample of the atmosphere in newly formed
ice.
When the snow gets packed down
by subsequent layers, the space between the
crystals is eventually sealed off, trapping a
small sample of the atmosphere in newly formed
ice.
By understanding the underlying physics producing the emissivity difference between these channels, this emissivity difference can be used to infer the relative concentration of
small ice crystals.
This may suggest that for a given optical thickness, the influence of particle shape on the radiative forcing caused
by a cloud composed of
small ice crystals can be negligible.