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  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2010
    In:  Journal of Geophysical Research Vol. 115, No. C5 ( 2010-05-07)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 115, No. C5 ( 2010-05-07)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2010
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    SSG: 16,13
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2014
    In:  Global Biogeochemical Cycles Vol. 28, No. 10 ( 2014-10), p. 1129-1148
    In: Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 28, No. 10 ( 2014-10), p. 1129-1148
    Abstract: Late summer NCP in the central Arctic Ocean by multiple approaches High NCP in the marginal sea ice zone and low NCP in the central basins Basin‐specific variability coupled to sea ice cover and nutrient supply
    Type of Medium: Online Resource
    ISSN: 0886-6236 , 1944-9224
    URL: Issue
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2014
    detail.hit.zdb_id: 2021601-4
    SSG: 12
    SSG: 13
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1985
    In:  Journal of Geophysical Research: Oceans Vol. 90, No. C5 ( 1985-09-20), p. 9194-9198
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 90, No. C5 ( 1985-09-20), p. 9194-9198
    Abstract: We report precise measurements of salinity, chlorinity, alkalinity, calcium, and sulphate in various types of sea ice collected at the Canadian Expedition to Study the Alpha Ridge (CESAR) Ice Camp in the Arctic Ocean and in both first‐year and multiyear ice collected in Fram Strait. Several of the samples showed some relative enrichment of alkalinity and sulphate compared to what would be observed in seawater of the same salinity. The relative enrichment was quite varied and did not correspond quantitatively with what has been observed in sea ice produced in the laboratory. Our results indicate that the temperature and salinity history of sea ice must be crucial in determining the relative composition of salts in natural sea ice and that quantitative geochemical predictions based on the composition of sea ice produced in the laboratory or on a particular specimen of natural sea ice must be made with caution.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1985
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    detail.hit.zdb_id: 3094268-8
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    SSG: 16,13
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2009
    In:  Journal of Geophysical Research Vol. 114, No. C1 ( 2009-01-03)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 114, No. C1 ( 2009-01-03)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2009
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  • 5
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2004
    In:  Journal of Geophysical Research Vol. 109, No. C1 ( 2004)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 109, No. C1 ( 2004)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2004
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    SSG: 16,13
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2004
    In:  Journal of Geophysical Research Vol. 109, No. C6 ( 2004)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 109, No. C6 ( 2004)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2004
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    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
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    detail.hit.zdb_id: 3094268-8
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    SSG: 16,13
    Location Call Number Limitation Availability
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1991
    In:  Journal of Geophysical Research: Oceans Vol. 96, No. C9 ( 1991-09-15), p. 16679-16687
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 96, No. C9 ( 1991-09-15), p. 16679-16687
    Abstract: Total carbonate data from the southern Weddell Sea, collected during the Swedish Antarctic Expedition in 1988–1989, has been investigated with respect to its content of anthropogenic carbon dioxide. The measured data was corrected for decay of organic matter by the use of the apparent oxygen utilization and the ratio of carbon to oxygen in organic matter. Correction due to precipitation or dissolution of metal carbonate was not found to be necessary from alkalinity and calcium data. With a combination of the water mass mixing conditions and the atmosphere‐ocean carbon dioxide exchange, the anthropogenic input of carbon dioxide has been estimated. The anthropogenic carbon dioxide mean concentration varies in the different water masses as a result of the mixing conditions, from about 36 μmol/kg in the Ice Shelf Water to 8 μmol/kg in the Antarctic Bottom Water. The data were combined with oceanographic information in order to elucidate the ventilation of carbon dioxide in the Weddell Sea. With the outflow of Ice Shelf Water from the Filchner Depression equal to 0.7 × 10 6 m 3 /s (Foldvik et al., 1985), the annual transport of anthropogenic carbon amounts to 8 × 10 12 g for this special area. There are indications of other areas with significant deep water formation, but it is unlikely for these to add more than 2 times that of the Filchner Depression. This results in a total sequestering in the Weddell Sea of less than 1% of the annual anthropogenic emission of about 5.5 Gt C.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1991
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    detail.hit.zdb_id: 710256-2
    detail.hit.zdb_id: 2016804-4
    detail.hit.zdb_id: 3094181-7
    detail.hit.zdb_id: 3094219-6
    detail.hit.zdb_id: 3094167-2
    detail.hit.zdb_id: 2220777-6
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
    Location Call Number Limitation Availability
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2008
    In:  Journal of Geophysical Research Vol. 113, No. C8 ( 2008-08-07)
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 113, No. C8 ( 2008-08-07)
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2008
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    SSG: 16,13
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2002
    In:  Geophysical Research Letters Vol. 29, No. 17 ( 2002-09), p. 16-1-16-4
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 29, No. 17 ( 2002-09), p. 16-1-16-4
    Type of Medium: Online Resource
    ISSN: 0094-8276
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2002
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    detail.hit.zdb_id: 7403-2
    SSG: 16,13
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  • 10
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2013
    In:  Journal of Geophysical Research: Oceans Vol. 118, No. 1 ( 2013-01), p. 410-421
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 118, No. 1 ( 2013-01), p. 410-421
    Abstract: Two different regions for the formation of AO upper halocline Brine enriched bottom water produce AO upper halocline Change in summer sea ice coverage can be important
    Type of Medium: Online Resource
    ISSN: 2169-9275 , 2169-9291
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2013
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    SSG: 16,13
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