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  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1990
    In:  Journal of Geophysical Research: Oceans Vol. 95, No. C11 ( 1990-11-15), p. 20147-20165
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 95, No. C11 ( 1990-11-15), p. 20147-20165
    Abstract: Deep ventilation and water mass transformation processes in the North Atlantic, on decadal time scales, are illustrated by the evolving distribution patterns of anthropogenic tritium and radiocarbon. Data from two quasisynoptic surveys of the interior of the North Atlantic, the Geochemical Ocean Sections Study (GEOSECS) and complementary oceanographic observation projects in 1972, and the Transient Tracers in the Oceans (TTO) in 1981 and 1983, are presented in comparative cross sections and maps representing conditions roughly one and two decades, respectively, after the first major tracer injections. The discussion emphasizes comparisons of the decay corrected tritium concentration fields, which show several distinct regimes of transient evolution, including examples of surprising constancy in some regional patterns. While largely supportive of previous qualitative ideas about transport patterns, these results also suggest that the patterns of deep water injection in high latitudes must have undergone a major change around or soon after the time of GEOSECS (1972), involving a major increase in supply of Upper North Atlantic Deep Water. The near‐surface waters show strong signatures of tropical (low tritium) influence in the southwestern and western part of the subtropical gyre, while the northeastern part is influenced by continued tritium input from Arctic surface waters. Strong evidence for distinct sub‐basin‐scale interior circulation domains is found in the fact that the major distribution regime transitions seen in the GEOSECS data are observed again in TTO, and thus maintained through the second decade of the transient. The radiocarbon data set, which reflects the addition to the natural background distribution, supports the significance also on longer time scales of the mid‐depth regime transition around 30°N latitude.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1990
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1983
    In:  Journal of Geophysical Research: Oceans Vol. 88, No. C1 ( 1983-01-20), p. 763-769
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 88, No. C1 ( 1983-01-20), p. 763-769
    Abstract: Tritium samples have been analyzed from several cross‐equatorial transects in the Pacific under the NORPAX and EPOCS programs. Together with earlier sections from the GEOSECS program, they allow description of the equatorial Pacific tritium transient over a period extending between approximately the tenth and the fifteenth year after the major nuclear tests. South of the equator within the upper water layers at temperatures above 16°, an increase of 25–60% in the decay‐corrected tritium concentration is found. A northern hemisphere source for the tritium increase is unequivocally indicated, but the details of the exchange are as yet uncertain. The tritium transient evolution is consistent with recent suggestions that the net cross‐equatorial oceanic heat transport in the Pacific is small on the scale of the global atmospheric heat transport processes. An additional result relevant to the equatorial heat budget is that the tritium data put a lower bound of 16° on the temperature of the water up welling at the equator.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1983
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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1970
    In:  Journal of Geophysical Research Vol. 75, No. 12 ( 1970-04-20), p. 2323-2327
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 75, No. 12 ( 1970-04-20), p. 2323-2327
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1970
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  • 4
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1987
    In:  Journal of Geophysical Research: Oceans Vol. 92, No. C4 ( 1987-04-15), p. 3769-3777
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 92, No. C4 ( 1987-04-15), p. 3769-3777
    Abstract: Application of mass balances of 18 O, tritium and salt, plus 14 C data show that the deep Eurasian Basin exchanges water with the subarctic Atlantic Ocean on a time scale of 10 to 100 years, while the deep Canada Basin has an exchange time scale of about 700 years. Only small fractions, less than 10 to 15% of the deep waters, originate from the shelves. The deep Canada Basin cannot consist of fossil water from glacial time or from the latest cool climate spell, just 100 to 300 years ago.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1987
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  • 5
    Online Resource
    Online Resource
    Stockholm University Press ; 1970
    In:  Tellus Vol. 22, No. 4 ( 1970-08), p. 463-465
    In: Tellus, Stockholm University Press, Vol. 22, No. 4 ( 1970-08), p. 463-465
    Type of Medium: Online Resource
    ISSN: 0040-2826 , 2153-3490
    URL: Issue
    Language: English
    Publisher: Stockholm University Press
    Publication Date: 1970
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  • 6
    Online Resource
    Online Resource
    Stockholm University Press ; 1970
    In:  Tellus A: Dynamic Meteorology and Oceanography Vol. 22, No. 4 ( 1970-01-01), p. 463-
    In: Tellus A: Dynamic Meteorology and Oceanography, Stockholm University Press, Vol. 22, No. 4 ( 1970-01-01), p. 463-
    Type of Medium: Online Resource
    ISSN: 1600-0870
    Language: Unknown
    Publisher: Stockholm University Press
    Publication Date: 1970
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  • 7
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1977
    In:  Journal of Geophysical Research Vol. 82, No. 9 ( 1977-03-20), p. 1454-1454
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 82, No. 9 ( 1977-03-20), p. 1454-1454
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1977
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  • 8
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1969
    In:  Journal of Geophysical Research Vol. 74, No. 18 ( 1969-08-20), p. 4535-4543
    In: Journal of Geophysical Research, American Geophysical Union (AGU), Vol. 74, No. 18 ( 1969-08-20), p. 4535-4543
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1969
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  • 9
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1982
    In:  Journal of Geophysical Research: Oceans Vol. 87, No. C3 ( 1982-03-20), p. 2035-2043
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 87, No. C3 ( 1982-03-20), p. 2035-2043
    Abstract: The time function of bomb tritium concentrations in river runoff to the Arctic Ocean has been reconstructed from published data on tritium in precipitation 1959–1975. Tritium measurements on oceanic samples through the halocline exhibit strong linear relationships between tritium concentrations (TU values) and salinity. These waters thus look like binary mixtures of Atlantic source water and freshwater runoff. Combining these data, the vintage of the freshwater component in the Arctic Basin has been determined assuming no other major tritium source. The relation indicates the average age of the freshwater component to be 11±1 years in the Nansen Basin and the outflow and somewhat higher in the Canada Basin. According to tritium/salinity data, a surface layer of 10–60 m is affected by sea ice melting and freezing in the Nansen Basin, and the thickness of this layer increases to 150–170 m toward the Canada Basin. There is tritium also in the deeper waters, the unmixed Atlantic water, which points at residence times for that water not to exceed 17 years. The appendix is available with the entire article on microfiche. Order from American Geophysical Union, 2000 Florida Avenue, N.W., Washington, D.C. 20009. Document J81‐012; $1.00, payment must accompany order.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1982
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  • 10
    In: Earth and Planetary Science Letters, Elsevier BV, Vol. 87, No. 4 ( 1988-3), p. 379-389
    Type of Medium: Online Resource
    ISSN: 0012-821X
    RVK:
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1988
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