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Xiaolei Niu and Rachel T. Pinker

Global Product) and at 5-km spatial scales (using the MODIS level-2 Swath Product; Su et al. 2008 ). Information on atmospheric constituents, both water and ice cloud properties (cloud particle effective radius and optical properties), and surface albedo is used. The spectral SWR is retrieved for a multilayered atmosphere that accounts for surface elevation and for the representation of the vertical distribution of atmospheric variables. Since the publication of the Wang and Pinker (2009

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Sohey Nihashi, Kay I. Ohshima, and Noriaki Kimura

.1029/2005JC003327 . Fukamachi , Y. , and Coauthors , 2009 : Direct observations of sea-ice thickness and brine rejection off Sakhalin in the Sea of Okhotsk . Cont. Shelf Res. , 29 , 1541 – 1548 . Gradinger , R. R. , and M. E. M. Banmann , 1991 : Distribution of phytoplankton communities in relation to the large-scale hydrographical regime in the Fram Strait . Mar. Biol. , 111 , 311 – 321 . Grenfell , T. C. , and G. A. Maykut , 1977 : The optical properties of ice and snow in the

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