GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Years
  • 1
    Publication Date: 2018-01-19
    Description: Seasonal and spatial variability of dissolved Barium (Ba) in Amundsen Gulf, southeastern Beaufort Sea, was monitored over a full year from September 2007 to September 2008. Dissolved Ba displays a nutrient-type behavior: the maximum water column concentration is located below the surface layer. Highest Ba concentrations are typically observed at river mouths, the lowest concentrations are found in water masses of Atlantic origin. Barium concentrations decrease eastward through the Canadian Arctic Archipelago. Barite (BaSO4) saturation is reached at the maximum concentrations of dissolved Ba in the subsurface layer, whereas the remaining water column is undersaturated. A three end-member mixing model comprising freshwater from sea-ice melt and rivers, as well as upper halocline water, was used to establish their relative contributions to the Ba concentrations in the upper water column of the Amundsen Gulf. Based on water column and riverine Ba contributions, we assess the depletion of dissolved Ba by formation and concomitant sinking of biologically bound Ba (bio-Ba), from which we derive an estimate of the carbon export production. In the upper 50 m of the water column of Amundsen Gulf, riverine Ba accounts for up to 15% of the available dissolved Ba inventory, of which up to 20% is depleted by bio-Ba formation and export. Since riverine inputs and Ba export occur concurrently, the seasonal variability of dissolved Ba in the upper water column is moderate. Assuming a fixed organic carbon to bio-Ba flux ratio, carbon export out of the surface layer is estimated at 1.8{plus minus}0.45 mol C m‑2 yr‑1. We propose a climatological carbon budget for the Amundsen Gulf.
    Type: Article , PeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    facet.materialart.
    Unknown
    University of Manitoba
    In:  EPIC3Arctic-ICE 2011 field report: A sea ice-based study in Resolute Passage, NU, Canada., Winnipeg, University of Manitoba, 124 p., pp. 36-45
    Publication Date: 2014-04-15
    Repository Name: EPIC Alfred Wegener Institut
    Type: Inbook , peerRev
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © Oceanography Society, 2011. This article is posted here by permission of Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 24 no. 3 (2011): 202–218, doi:10.5670/oceanog.2011.72.
    Description: The porous nature of sea ice not only provides a habitat for ice algae but also opens a pathway for exchanges of organic matter, nutrients, and gases with the seawater below and the atmosphere above. These constituents permeate the ice cover through air-ice gas exchange, brine drainage, seawater entrainment into the ice, and air-sea gas exchange within leads and polynyas. The central goal in sea ice biogeochemistry since the 1980s has been to discover the physical, biological, and chemical rates and pathways by which sea ice affects the distribution and storage of biogenic gases (namely CO2, O2, and dimethyl sulfide) between the ocean and the atmosphere. Historically, sea ice held the fascination of scientists for its role in the ocean heat budget, and the resulting view of sea ice as a barrier to heat and mass transport became its canonical representation. However, the recognition that sea ice contains a vibrant community of ice-tolerant organisms and strategic reserves of carbon has brought forward a more nuanced view of the "barrier" as an active participant in polar biogeochemical cycles. In this context, the organisms and their habitat of brine and salt crystals drive material fluxes into and out of the ice, regulated by liquid and gas permeability. Today, scientists who study sea ice are acutely focused on determining the flux pathways of inorganic carbon, particulate organics, climate-active gases, excess carbonate alkalinity, and ultimately, the role of all of these constituents in the climate system. Thomas and Dieckmann (2010) recently reviewed sea ice biogeochemistry, and so we do not attempt a comprehensive review here. Instead, our goal is to provide a historical perspective, along with some recent discoveries and observations to highlight the most outstanding questions and possibly useful avenues for future research.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 120 (2015): 3542-3566, doi:10.1002/2014JC010620.
    Description: We present the results of a 6 week time series of carbonate system and stable isotope measurements investigating the effects of sea ice on air-sea CO2 exchange during the early melt period in the Canadian Arctic Archipelago. Our observations revealed significant changes in sea ice and sackhole brine carbonate system parameters that were associated with increasing temperatures and the buildup of chlorophyll a in bottom ice. The warming sea-ice column could be separated into distinct geochemical zones where biotic and abiotic processes exerted different influences on inorganic carbon and pCO2 distributions. In the bottom ice, biological carbon uptake maintained undersaturated pCO2 conditions throughout the time series, while pCO2 was supersaturated in the upper ice. Low CO2 permeability of the sea ice matrix and snow cover effectively impeded CO2 efflux to the atmosphere, despite a strong pCO2 gradient. Throughout the middle of the ice column, brine pCO2 decreased significantly with time and was tightly controlled by solubility, as sea ice temperature and in situ melt dilution increased. Once the influence of melt dilution was accounted for, both CaCO3 dissolution and seawater mixing were found to contribute alkalinity and dissolved inorganic carbon to brines, with the CaCO3 contribution driving brine pCO2 to values lower than predicted from melt-water dilution alone. This field study reveals a dynamic carbon system within the rapidly warming sea ice, prior to snow melt. We suggest that the early spring period drives the ice column toward pCO2 undersaturation, contributing to a weak atmospheric CO2 sink as the melt period advances.
    Description: We acknowledge support from the Polar Continental Shelf Program (PCSP) of Natural Resources Canada, the Natural Sciences and Engineering Research Council of Canada, the Northern Scientific Training Program, Canada Economic Development, and Fisheries and Oceans Canada.
    Description: 2015-11-19
    Keywords: Sea ice ; Carbon cycling ; CO2 ; Brines ; Stable isotopes ; Arctic Ocean
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2023-05-12
    Description: We conducted a six-week investigation of the sea ice inorganic carbon system during the winter-spring transition in the Canadian Arctic Archipelago. Samples for the determination of sea ice geochemistry were collected in conjunction with physical and biological parameters as part of the 2010 Arctic-ICE (Arctic - Ice-Covered Ecosystem in a Rapidly Changing Environment) program, a sea ice-based process study in Resolute Passage, Nunavut. The goal of Arctic-ICE was to determine the physical-biological processes controlling the timing of primary production in Arctic landfast sea ice and to better understand the influence of these processes on the drawdown and release of climatically active gases. The field study was conducted from 1 May to 21 June, 2010.
    Keywords: Arctic-ICE; Arctic-ICE2010; Arctic - Ice-Covered Ecosystem in a Rapidly Changing Environment; ICE; Ice station; Resolute Passage, Nunavut
    Type: Dataset
    Format: application/zip, 5 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2023-05-12
    Keywords: Alkalinity, total; Arctic-ICE; Arctic-ICE2010; Arctic - Ice-Covered Ecosystem in a Rapidly Changing Environment; Carbon, inorganic, total; Conductivity meter, WTW Cond 330i, Nova Analytics; Coulometric titration; DATE/TIME; Depth, bottom/max; Freeboard; ICE; Ice station; Identification; Investigator; LATITUDE; LONGITUDE; Mass spectrometer Finnigan Delta Plus XL; Mass spectrometer GV Instruments Isoprime; Open-cell titration; Resolute Passage, Nunavut; Salinity, brine; Sea ice thickness; Snow thickness; δ13C, total inorganic carbon; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 344 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2023-05-12
    Keywords: 2,4,6-Tribromoanisole in air; 2,4-Dibromoanisole in air; alpha-Hexachlorocyclohexane in air; ArcticNet; Area/locality; Beaufort Sea; Campaign; CCGSA_1; CCGSA_1a_st; CCGSA_1b_st; CCGSA_4-10_CFL08; CCGSA_5-9_st; CCGS Amundsen; Circumpolar Flaw Lead Leg 4-10a; DATE/TIME; Date/time end; Event label; gamma-Hexachlorocyclohexane in air; Hexachlorobenzene, standard deviation; Hexachlorobenzene in air; Hexachlorocyclohexane, standard deviation; Hudson Bay; Labrador Sea; MULT; Multiple investigations; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 53 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2023-05-12
    Keywords: 2,4,6-Tribromoanisole; 2,4-Dibromoanisole; alpha-Hexachlorocyclohexane; ArcticNet; Area/locality; Beaufort Sea; Campaign; CCGSA_1; CCGSA_1a_st; CCGSA_1b_st; CCGSA_4-10_CFL08; CCGSA_5-9_st; CCGS Amundsen; Circumpolar Flaw Lead Leg 4-10a; DATE/TIME; Date/time end; Event label; gamma-Hexachlorocyclohexane; Hexachlorobenzene; Hexachlorobenzene, standard deviation; Hexachlorocyclohexane, standard deviation; Hudson Bay; Labrador Sea; MULT; Multiple investigations; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 52 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2023-05-12
    Keywords: 2,4,6-Tribromoanisole in air; 2,4-Dibromoanisole in air; alpha-Hexachlorocyclohexane in air; ArcticNet; Beaufort Sea; Campaign; CCGSA_1; CCGSA_1_4-5; CCGSA_1_6-7; CCGSA_1_8-9; CCGSA_4-10_15-17; CCGSA_4-10_20-22; CCGSA_4-10_25-27; CCGSA_4-10_28-30; CCGSA_4-10_31-33; CCGSA_4-10_34-36; CCGSA_4-10_37-39; CCGSA_4-10_40-42; CCGSA_4-10_43-45; CCGSA_4-10_46-48; CCGSA_4-10_49-51; CCGSA_4-10_52-54; CCGSA_4-10_55-57; CCGSA_4-10_58-60; CCGSA_4-10_CFL08; CCGS Amundsen; Circumpolar Flaw Lead Leg 4-10a; Date/Time of event; Date/Time of event 2; Event label; gamma-Hexachlorocyclohexane in air; Height above sea level; Hexachlorobenzene in air; Hudson Bay; Latitude of event; Longitude of event; MULT; Multiple investigations; Northwestern Passages; Recovery; Sample code/label; Station label
    Type: Dataset
    Format: text/tab-separated-values, 338 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2023-05-12
    Keywords: ArcticNet; Beaufort Sea; Campaign; CCGSA_1; CCGSA_1_4-5; CCGSA_1_6-7; CCGSA_1_8-9; CCGSA_4-10_15-17; CCGSA_4-10_20-22; CCGSA_4-10_25-27; CCGSA_4-10_28-30; CCGSA_4-10_31-33; CCGSA_4-10_34-36; CCGSA_4-10_37-39; CCGSA_4-10_40-42; CCGSA_4-10_43-45; CCGSA_4-10_46-48; CCGSA_4-10_49-51; CCGSA_4-10_52-54; CCGSA_4-10_55-57; CCGSA_4-10_58-60; CCGSA_4-10_CFL08; CCGS Amundsen; Circumpolar Flaw Lead Leg 4-10a; Date/Time of event; Date/Time of event 2; Event label; Hudson Bay; Latitude of event; Longitude of event; MULT; Multiple investigations; Northwestern Passages; Sample code/label; Station label; Surface description; Temperature, air; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 102 data points
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...