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  • 1995-1999  (3)
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Language
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  • 1995-1999  (3)
Year
  • 1
    Online Resource
    Online Resource
    Journal of Marine Research/Yale ; 1999
    In:  Journal of Marine Research Vol. 57, No. 4 ( 1999-7-1), p. 693-713
    In: Journal of Marine Research, Journal of Marine Research/Yale, Vol. 57, No. 4 ( 1999-7-1), p. 693-713
    Type of Medium: Online Resource
    ISSN: 1543-9542 , 0022-2402
    Language: Unknown
    Publisher: Journal of Marine Research/Yale
    Publication Date: 1999
    detail.hit.zdb_id: 410655-6
    detail.hit.zdb_id: 2066603-2
    SSG: 12
    Location Call Number Limitation Availability
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1998
    In:  Journal of Geophysical Research: Oceans Vol. 103, No. C12 ( 1998-11-15), p. 27795-27807
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 103, No. C12 ( 1998-11-15), p. 27795-27807
    Abstract: In low‐saline estuaries, “juvenile freshwater,” that is, freshwater trapped by the seasonal thermal stratification, may be used as an almost neutrally buoyant natural tracer for dispersion studies. Most of the juvenile freshwater supplied to the Baltic proper enters the northern parts by runoff from rivers and outflow of low‐saline water from the Bothnian Sea. The mean monthly spatial distribution of juvenile freshwater in the Baltic proper in the period April to August is studied using historical hydrographic data. Month‐to‐month changes of the distribution reveal a fast southward spreading that only partly can be explained by the quite slow mean circulation in the Baltic proper. Most of the spreading is probably due to currents forced by fluctuating winds. In early spring, when the surface temperature is around the temperature of maximal density, the spreading of juvenile freshwater may initiate the seasonal stratification, which in turn starts the spring bloom. The spreading route of juvenile freshwater in early spring, as deduced in this paper, is in qualitative agreement with the spatial progress of the observed time for the start of the spring bloom of phytoplankton. The use of juvenile freshwater as a tracer should help in the interpretation of the spreading of tracers (e.g., pollutants) from local sources, as well as helping to verify recipes for calculating the spread of tracer clouds by different mechanisms. The monthly averaged spatial distributions of juvenile freshwater in the Baltic proper presented in this paper should be useful for testing dispersion properties of state‐of‐the‐art three‐dimensional ocean circulation models.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1998
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    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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  • 3
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1997
    In:  Journal of Geophysical Research: Oceans Vol. 102, No. C4 ( 1997-04-15), p. 8657-8662
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 102, No. C4 ( 1997-04-15), p. 8657-8662
    Abstract: Local buoyancy supply associated with the pulsed horizontal advection of water of lower salinity at the sea surface can initiate the development of a shallow thermocline in spring. This process has been studied with an analysis of historical hydrographic data from the central parts of the Baltic proper and numerical experiments with a seasonal pycnocline model. It is shown that this situation occurs in the Baltic Sea when the temperature of the surface water is below the temperature of maximum water density and the buoyancy flux due to heating at the sea surface is negative.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1997
    detail.hit.zdb_id: 2033040-6
    detail.hit.zdb_id: 3094104-0
    detail.hit.zdb_id: 2130824-X
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 2016810-X
    detail.hit.zdb_id: 2403298-0
    detail.hit.zdb_id: 2016800-7
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 161667-5
    detail.hit.zdb_id: 2969341-X
    detail.hit.zdb_id: 161665-1
    detail.hit.zdb_id: 3094268-8
    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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