Effects of temperature on the microstructure of first‐year Arctic sea ice

By B. Light, G. Maykut, T. Grenfell. 2003

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Thermal conductivity of landfast Antarctic and Arctic sea ice (2007, unknown): “While this bubbly ice picture is appropriate for MY ice, recent work shows that in FY ice, air bubbles are almost entirely found within brine inclusions [Light et al., 2003].”
A review of snow and ice albedo and the development of a new physically based broadband albedo parameterization (2010, background): “[24] The albedo of glacier, lake and sea ice is influenced by the same factors as snow with the exception that, instead of being governed by grain size, the frequency and location of scattering events (air-ice interfaces) are determined by the size and distribution of air bubbles, brine inclusions a”