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  • 2010-2014  (6)
Publikationsart
Schlagwörter
Erscheinungszeitraum
Jahr
  • 1
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    Unbekannt
    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
    Publikationsdatum: 2023-12-13
    Beschreibung: 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.
    Schlagwort(e): 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
    Materialart: Dataset
    Format: text/tab-separated-values, 174 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    Unbekannt
    PANGAEA
    In:  Supplement to: Palmer, Molly A; Arrigo, Kevin R; Mundy, Christopher John; Ehn, Jens K; Gosselin, Michel; Barber, David G; Martin, Johannie; Alou, Eva; Roy, Suzanne; Tremblay, Jean-Éric (2011): Spatial and temporal variation of photosynthetic parameters in natural phytoplankton assemblages in the Beaufort Sea, Canadian Arctic. Polar Biology, 34(12), 1915-1928, https://doi.org/10.1007/s00300-011-1050-x
    Publikationsdatum: 2024-04-27
    Beschreibung: During summer 2008, as part of the Circumpolar Flaw Lead system study, we measured phytoplankton photosynthetic parameters to understand regional patterns in primary productivity, including the degree and timescale of photoacclimation and how variability in environmental conditions influences this response. Photosynthesis-irradiance measurements were taken at 15 sites primarily from the depth of the subsurface chlorophyll a (Chl a) maximum (SCM) within the Beaufort Sea flaw lead polynya. The physiological response of phytoplankton to a range of light levels was used to assess maximum rates of carbon (C) fixation (P*m), photosynthetic efficiency (alpha*), photoacclimation (Ek), and photoinhibition (beta*). SCM samples taken along a transect from under ice into open water exhibited a 〉3-fold increase in alpha* and P*m, showing these parameters can vary substantially over relatively small spatial scales, primarily in response to changes in the ambient light field. Algae were able to maintain relatively high rates of C fixation despite low light at the SCM, particularly in the large (〉5 µm) size fraction at open water sites. This may substantially impact biogenic C drawdown if species composition shifts in response to future climate change. Our results suggest that phytoplankton in this region are well acclimated to existing environmental conditions, including sea ice cover, low light, and nutrient pulses. Furthermore, this photoacclimatory response can be rapid and keep pace with a developing SCM, as phytoplankton maintain photosynthetic rates and efficiencies in a narrow ''shade-acclimated'' range.
    Schlagwort(e): International Polar Year (2007-2008); IPY
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2024-04-27
    Schlagwort(e): Amundsen Gulf, Canada; Chlorophyll a; Darnley_Bay08; DATE/TIME; DEPTH, water; Depth of the euphotic zone; Event label; Fixation of carbon in chlorophyll; International Polar Year 2007-2008; IPY-4; Light absorption by phytoplankton per chlorophyll a; Mixed layer depth; MULT; Multiple investigations; Nitrate; Photoinhibition in carbon per chlorophyll a; Photosynthetic efficiency, carbon production; Quantum yield; Radiation, photosynthetically active; Ratio; Sample comment; Sample type; Temperature, water
    Materialart: Dataset
    Format: text/tab-separated-values, 104 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2024-04-27
    Schlagwort(e): Ammonium; Amundsen Gulf, Canada; Beaufort Sea; CCGSA_4-10_CFL08; CCGS Amundsen; CFL08_1200; CFL08_1216-1; CFL08_405B-1; CFL08_421-2; CFL08_435; CFL08_6006-2; Chlorophyll a; Circumpolar Flaw Lead Leg 4-10a; Darnley_Bay08; DATE/TIME; DEPTH, water; Depth of the euphotic zone; Elevation, mean; Event label; Franklin_Bay08; International Polar Year 2007-2008; IPY-4; Latitude of event; Longitude of event; Mixed layer depth; MOOR; Mooring; MULT; Multiple investigations; Nitrate and Nitrite; Phosphate; Radiation, photosynthetically active; Salinity; Silicate; Station label; Temperature, water
    Materialart: Dataset
    Format: text/tab-separated-values, 164 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2019-09-23
    Beschreibung: During two consecutive cruises to the Eastern Central Arctic in late summer 2012, we observed floating algal aggregates in the melt-water layer below and between melting ice floes of first-year pack ice. The macroscopic (1-15 cm in diameter) aggregates had a mucous consistency and were dominated by typical ice-associated pennate diatoms embedded within the mucous matrix. Aggregates maintained buoyancy and accumulated just above a strong pycnocline that separated meltwater and seawater layers. We were able, for the first time, to obtain quantitative abundance and biomass estimates of these aggregates. Although their biomass and production on a square metre basis was small compared to ice-algal blooms, the floating ice-algal aggregates supported high levels of biological activity on the scale of the individual aggregate. In addition they constituted a food source for the ice-associated fauna as revealed by pigments indicative of zooplankton grazing, high abundance of naked ciliates, and ice amphipods associated with them. During the Arctic melt season, these floating aggregates likely play an important ecological role in an otherwise impoverished near-surface sea ice environment. Our findings provide important observations and measurements of a unique aggregate-based habitat during the 2012 record sea ice minimum year
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Publikationsdatum: 2019-07-17
    Beschreibung: During two consecutive cruises to the Eastern Central Arctic in late summer 2012, we observed floating algal aggregates in the melt-water layer below and between melting ice floes of first-year pack ice. The macroscopic (1 – 15 cm in diameter) aggregates had a mucous consistency and were dominated by typical ice-associated pennate diatoms embedded within the mucous matrix. Aggregates maintained buoyancy and accumulated just above a strong pycnocline that separated meltwater and seawater layers. We were able, for the first time, to obtain quantitative abundance and biomass estimates of these aggregates. Although their biomass and production on a square metre basis was small compared to ice-algal blooms, the floating ice-algal aggregates supported high levels of biological activity on the scale of the individual aggregate. In addition they constituted a food source for the ice-associated fauna as revealed by pigments indicative of zooplankton grazing, high abundance of naked ciliates, and ice amphipods associated with them. During the Arctic melt season, these floating aggregates likely play an important ecological role in an otherwise impoverished near-surface sea ice environment. Our findings provide important observations and measurements of a unique aggregate-based habitat during the 2012 record sea ice minimum year.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Format: application/pdf
    Standort Signatur Einschränkungen Verfügbarkeit
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