reflective properties of white sea ice and snow
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2016
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Abstract
White ice (ice with a highly scattering granular layer on top of its surface)
and snow-covered ice occupy a large part of the sea ice area in the Arctic,
the former in summer, the latter in the cold period. The inherent optical
properties (IOPs) and the reflectance of these types of ice are considered
from the point of view of the light scattering and radiative transfer
theories. The IOPs – the extinction and absorption coefficients and the
scattering phase function – are derived with the assumption that both the snow cover and the scattering layer of white ice are random mixtures of air and
ice with the characteristic grain size significantly larger than
the wavelength of incident light. Simple analytical formulas are put forward to
calculate the bidirectional reflectance factor (BRF), albedo at direct
incidence (the directional–hemispherical reflectance), and albedo at diffuse incidence (the bihemispherical reflectance). The optical model developed is verified with the data of the in situ measurements made during the
R/V Polarstern expedition ARK-XXVII/3 in 2012.
| Reference Key |
malinka2016thereflective
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|---|---|
| Authors | ;A. Malinka;E. Zege;G. Heygster;L. Istomina |
| Journal | journal of applied polymer science |
| Year | 2016 |
| DOI |
10.5194/tc-10-2541-2016
|
| URL | |
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