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The spatial distribution of solar radiation under a melting Arctic sea ice cover
Author(s) -
Frey Karen E.,
Perovich Donald K.,
Light Bonnie
Publication year - 2011
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2011gl049421
Subject(s) - sea ice , arctic , spatial distribution , arctic ice pack , environmental science , climatology , geology , the arctic , radiation , cover (algebra) , cryosphere , oceanography , atmospheric sciences , remote sensing , physics , mechanical engineering , quantum mechanics , engineering
The sea ice cover of the Chukchi and Beaufort Seas is currently undergoing a fundamental shift from multiyear ice to first‐year ice. Field observations of sea ice physical and optical properties were collected in this region during June–July 2010, revealing unexpectedly complex spatial distributions of solar radiation under the melt‐season ice cover. Based on our optical measurements of first‐year ice, we found the under‐ice light field in the upper ocean to be spatially heterogeneous and dependent on wavelength, ice thickness, and the areal and geometric distribution of melt ponded and bare ice surfaces. Much of the observed complexity in radiation fields arose because the transmission of light through ponded ice was generally an order of magnitude greater than through bare, unponded ice. Furthermore, while many sites exhibited a consistent, exponential decay in light transmission through both ponded and bare ice surfaces, light transmission under bare ice was also observed to increase with depth (reaching maximum values ∼5–10 m below the bottom of the ice). A simple geometric model shows these transmission peaks are a result of scattering in the ice and the interspersion of bare and ponded sea ice surfaces. These new observations of complex radiation fields beneath melt‐season first‐year sea ice have significant implications for biological production, biogeochemical processes, and the heat balance of sea ice and under‐ice ocean waters and should be carefully considered when modeling these sea ice‐related phenomena.