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enough light levels for optimistic web photosynthesis occurs ncurrently with the melt progression in late spring as icesurface situations shift from a extremely reflective snow ver to a much less reflective mosaic of bare ice and soften ponds. However, spatial variability in icesurface traits, i.e. snow thickness or soften pond distributions, and the next impression on transmitted PAR makes estimates of lightlimited major manufacturing difficult presently of months. To quantify the rise of spectral mild transmission as a function of melting seaice floor and altering icealgae ncentration within the ice backside, a remotely operated vehicle outfitted with hyperspectral radiometers was deployed during the GreenEdge icecamp campaign in JuneJuly in Baffin Bay. Horizontal transects of m length at m depth and vertical profiles, to a depth of fifty m, had been repeatedly carried out beneath the ice wl with altering portions of snow, ice, melt ponds and ice algae. In this poster, we present an in depth dataset on the spatial and temporal progression of transmitted spectral irradiance and talk about the provision of PAR on average within the upper water lumn in relation to the modifications in the aforementioned variables. With decreased sea ice have me

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Daffy duck bugs bunny cartoon warner bros hawaiian shirt 1 Copy 2

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