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  • 1
    Publication Date: 2023-05-12
    Keywords: Amundsen Gulf, Canada; Chlorophyll a; Darnley_Bay08; DATE/TIME; Date/time end; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; Fluorometry (TURNER, 10-AU-005); Franklin_Bay08; International Polar Year 2007-2008; IPY-4; MULT; Multiple investigations; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 37 data points
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  • 2
    Publication Date: 2023-07-10
    Keywords: Amundsen Gulf, Canada; Apherusa glacialis; Calanoida; Darnley_Bay08; DATE/TIME; Date/time end; Event label; Franklin_Bay08; Gammarus wilkitzkii; International Polar Year 2007-2008; IPY-4; Ischyrocerus sp.; MULT; Multiple investigations; Onisimus glacialis; Onisimus spp.; Pisces
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 3
    Publication Date: 2023-07-10
    Keywords: Acartia longiremis; Aglantha digitale; Amundsen Gulf, Canada; Calanus glacialis; Calanus hyperboreus; Clione limacina; Copepoda, nauplii; Darnley_Bay08; DATE/TIME; Date/time end; Depth, bottom/max; Depth, top/min; DEPTH, water; Event label; Franklin_Bay08; Harpacticoida; Indeterminata; International Polar Year 2007-2008; IPY-4; Isopoda; Limacina helicina; MULT; Multiple investigations; Oithona similis; Pseudocalanus spp.
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 4
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    PANGAEA
    In:  Supplement to: Ehn, Jens K; Mundy, Christopher John; Barber, David G; Hop, Haakon; Rossnagel, Andrea L; Stewart, Jeremy (2011): Impact of horizontal spreading on light propagation in melt pond covered seasonal sea ice in the Canadian Arctic. Journal of Geophysical Research: Oceans, 116, C00G02, https://doi.org/10.1029/2010JC006908
    Publication Date: 2023-12-13
    Description: Melt pond covered sea ice is a ubiquitous feature of the summertime Arctic Ocean when meltwater collects in lower-lying areas of ice surfaces. Horizontal transects were conducted during June 2008 above and below landfast sea ice with melt ponds to characterize surface and bottom topography together with variations in transmitted spectral irradiance. We captured a rapid progression from a highly flooded sea ice surface with lateral drainage toward flaws and seal breathing holes to the formation of distinct melt ponds with steep edges. As the mass of the ice cover decreased due to meltwater drainage and rose upward with respect to the seawater level, the high-scattering properties of ice above the water level (i.e., white ice) were continuously regenerated, while pond waters remained transparent compared to underlying ice. The relatively stable albedos observed throughout the study, even as ice thickness decreased, were directly related to these surface processes. Transmission through the ice cover of incident irradiance in the 400-700 nm wave band ranged from 38% to 67% and from 5% to 16% beneath ponded and white ice, respectively. Our results show that this transmission varied not only as a function of surface type (melt ponds or white ice) areal coverage but also in relation to ice thickness and proximity to other surface types through the influence of horizontal spreading of light. Thus, in contrast to albedo, this implies that regional transmittance estimates need to consider melt pond size and shape distributions and variations in optical properties and thickness of the ice cover.
    Keywords: Amundsen Gulf, Canada; Darnley_Bay_Site1; Darnley_Bay_Site3; DATE/TIME; Event label; Franklin_Bay_Site2; Franklin_Bay_Site4; Freeboard; Ice draft; ICEM; Ice measurement; International Polar Year (2007-2008); International Polar Year 2007-2008; IPY; IPY-4; Irradiance, incident; Irradiance, incident, photosynthetically active; Melt pond depth; Melt pond freeboard; Sample type; Sea ice thickness; Site; Transmittance; Transmittance, photosynthetically active; Water level
    Type: Dataset
    Format: text/tab-separated-values, 174 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Hop, Haakon; Mundy, Christopher John; Gosselin, Michel; Rossnagel, Andrea L; Barber, David G (2011): Zooplankton boom and ice amphipod bust below melting sea ice in the Amundsen Gulf, Arctic Canada. Polar Biology, 34(12), 1947-1958, https://doi.org/10.1007/s00300-011-0991-4
    Publication Date: 2023-12-13
    Description: Early summer in the Arctic with extensive ice melt and break-up represents a dramatic change for sympagic-pelagic fauna below seasonal sea ice. As part of the International Polar Year-Circumpolar Flaw Lead system study (IPY-CFL), this investigation quantified zooplankton in the meltwater layer below landfast ice and remaining ice fauna below melting ice during June (2008) in Franklin Bay and Darnley Bay, Amundsen Gulf, Canada. The ice was in a state of advanced melt, with fully developed melt ponds. Intense melting resulted in a 0.3- to 0.5-m-thick meltwater layer below the ice, with a strong halocline to the Arctic water below. Zooplankton under the ice, in and below the meltwater layer, was sampled by SCUBA divers. Dense concentrations (max. 1,400 ind./m**3) of Calanus glacialis were associated with the meltwater layer, with dominant copepodid stages CIV and CV and high abundance of nauplii. Less abundant species included Pseudocalanus spp., Oithona similis and C. hyperboreus. The copepods were likely feeding on phytoplankton (0.5-2.3 mg Chl-a/m**3) in the meltwater layer. Ice amphipods were present at low abundance (〈10 ind./m**2) and wet biomass (〈0.2 g/m**2). Onisimus glacialis and Apherusa glacialis made up 64 and 51% of the total ice faunal abundance in Darnley Bay and Franklin Bay, respectively. During early summer, the autochthonous ice fauna becomes gradually replaced by allochthonous zooplankton, with an abundance boom near the meltwater layer. The ice amphipod bust occurs during late stages of melting and break-up, when their sympagic habitat is diminished then lost.
    Keywords: International Polar Year (2007-2008); IPY
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 6
    Publication Date: 2011-03-30
    Print ISSN: 0722-4060
    Electronic ISSN: 1432-2056
    Topics: Biology
    Published by Springer
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