Collaborative Research on Sunlight and the Arctic Atmosphere-Ice-Ocean System (AIOS) Hajo Eicken Univ. of Alaska Fairbanks Kathy Jones CRREL Bonnie Light.

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Collaborative Research on Sunlight and the Arctic Atmosphere-Ice-Ocean System (AIOS) Hajo Eicken Univ. of Alaska Fairbanks Kathy Jones CRREL Bonnie Light Univ. of Washington Rebecca Woodgate Univ. of Washington Don Perovich CRREL John Weatherly CRREL Kay Runciman Univ. of Washington The AIOS sunlight team Jeremy Harbeck UAF

Sunlight and the Arctic AIOS Goals 1.Enhance our understanding of the present role that solar radiation plays in the Arctic AIOS 2.Improve our ability to predict its future role. 3.Determine spatially and temporally the partitioning of solar energy Where does all the sunlight go?

Reflected Absorbed Transmitted Atmosphere Ice Ocean Where does all the sunshine go? Only three possible fates for sunlight reflected back to atmosphere absorbed in snow and ice transmitted to ocean Determine over large scale Incident Transmitted Incident = reflected + absorbed + transmitted How hard can it be? Reflected

Temporal and spatial variability May June July AugustSeptember

Region of Interest EASE grid over the Arctic Basin…from 1979 to 2007…daily Pan – Arctic over ocean All on 25 x 25 km EASE grid (Equal Area Scalable Earth) Generate description of solar partitioning Daily values from 1979 to 2007 of Incident solar energy Reflected solar energy Absorbed in snow and ice, Transmitted to ocean Spectral, integrated, PAR

Solar input to open water Incident solar, ice concentration, and albedo -> heat input Input: Incident (F r ) from ERA-40 Ice concentration (C) Water albedo (  ) = 0.07 Output: Solar input to the ocean (F w ) F w = F r (1 –  ) (1 – C) Assume ice is opaque, for now

27 year trend of annual ocean solar heat input Units are percent per year Increasing solar heat input in 85% of area

Next step: the ice Do the hard part Solar partitioning by ice Reflected Absorbed Transmitted Input from: process studies field experiments models satellites Snow depth and ice thickness distributions Timing of onset of melt and freezeup Seasonal evolution of ice albedo Pond evolution Every day, over the entire grid Dry snow Pond evolutionFall freezeup Melting snow Pond evolution

Outreach Synthesize and collaborate Scientific community Archived datasets Web site Map based One click to data Integrated datasets will benefit Sea ice mass balance Oceanography Atmospheric chemistry Large-scale modeling Future field planning Public General interest article on ice-albedo feedback Public lectures K-5 synthesis puzzles