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  • 1
    Electronic Resource
    Electronic Resource
    Direct determination of geostrophic drag coefficients at sea (1974)
    Springer
    Boundary layer meteorology 7 (1974), S. 323-329 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Geostrophic drag coefficients are obtained from direct measurements of the momentum flux and from an objective analysis of the synoptic pressure field by the method of least squares. At a site in the Kiel Bight, a mean geostrophic drag coefficient c g = 0.0223 was obtained with near neutral/ slightly unstable conditions and a surface Rossby Number of 1.2 × 109.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00240835
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    Paper (German National Licenses)
    Fulltext
  • 2
    Electronic Resource
    Electronic Resource
    The influence of sea waves on the wind profile (1978)
    Springer
    Boundary layer meteorology 14 (1978), S. 403-414 
    Details
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract From wind profile and wave measurements performed during the JONSWAP II experiment, relations between the dimensionless profile slope and the significant wave height are derived. It is shown that the wind profile is distorted by the waves especially in the vicinity of the water surface. The wave influence on the profile seems to be restricted to heights below about three wave heights. Above this level, the dimensionless profile slope is an approximately constant value corresponding to a drag coefficient of about 1.15 × 10−3.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF00121049
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    Paper (German National Licenses)
    Fulltext
  • 3
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    Eine Apparatur zur Messung des vertikalen Wind-, Temperatur- und Feuchteprofils über dem Ozean (1967)
    Bornträger
    Details
    Publication Date: 2022-06-29
    Description: During the 1965 Atlantic Expedition the R/V "Meteor" was stationed on the equator for several weeks. In order to obtain the vertical flux of heat and momentum vertical profiles of dry and wet bulb temperatures and of wind speed were measured. The water temperature, and the dry and wet bulb temperatures of aspirated psychrometers were taken by means of platinum resistance thermometers. The wind speeds were obtained by contact anemometers and small generator type anemometers. The instruments were mounted at heights between 1 m and 9 m at a meteorological buoy. Connected by floating cables the buoy lay 300 m away from the ship, free of its disturbances.
    Type: Article , PeerReviewed
    Format: text
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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