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  • 2010-2014  (5)
  • 1985-1989  (15)
Document type
Keywords
Publisher
Language
Years
Year
  • 11
    Online Resource
    Online Resource
    Bestimmung mesoskaliger Variabilitäten der Oberflächentemperatur und der Attenuation im Nordatlantik aus Satellitenmessungen (1987)
    Kiel
    Details Availability
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource (199 Seiten = 10 MB) , Illustrationen, Graphen, Karten
    URL: https://oceanrep.geomar.de/43064/
    Language: German
    Location Call Number Limitation Availability
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    GEOMAR CATALOGUE
    Link to Library Catalog
    get availability status
  • 12
    Online Resource
    Online Resource
    Über die Fehler bei der Bestimmung dynamischer Topographien aus Messungen mit XBT-Sonden (1985)
    Kiel
    Details Availability
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (96 Seiten = 11 MB) , Graphen, Karte
    Edition: 2020
    URL: https://oceanrep.geomar.de/34662/
    Language: German
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    GEOMAR CATALOGUE
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  • 13
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    Unknown
    Physical oceanography during POSEIDON cruise POS104/1 (2010)
    PANGAEA
    In:  Institut für Meereskunde, Christian-Albrechts-Universität, Kiel
    Details
    Publication Date: 2023-12-16
    Keywords: CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; PO104A; POS104/1; POS104/1_505; POS104/1_514; POS104/1_516; POS104/1_518; POS104/1_520; POS104/1_522; POS104/1_524; POS104/1_526; POS104/1_528; POS104/1_530; POS104/1_532; POS104/1_534; POS104/1_538; POS104/1_540; POS104/1_542; POS104/1_544; POS104/1_546; POS104/1_548; POS104/1_550; POS104/1_552; POS104/1_554; POS104/1_556; POS104/1_558; POS104/1_560; POS104/1_562; POS104/1_564; POS104/1_566; POS104/1_568; POS104/1_570; POS104/1_572; Poseidon; Pressure, water; Salinity; SFB133; South Atlantic Ocean; Temperature, water; Warmwassersphäre des Atlantiks
    Type: Dataset
    Format: text/tab-separated-values, 339308 data points
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    DATA PANGAEA
  • 14
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    Unknown
    Physical oceanography during POSEIDON cruise POS104_2 (2010)
    PANGAEA
    In:  Institut für Meereskunde, Christian-Albrechts-Universität, Kiel
    Details
    Publication Date: 2023-12-16
    Keywords: CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; PO104A; POS104/2; POS104/2_576; POS104/2_578; POS104/2_580; POS104/2_582; POS104/2_584; POS104/2_586; POS104/2_588; POS104/2_590; POS104/2_592; POS104/2_594; POS104/2_596; POS104/2_598; POS104/2_600; POS104/2_602; POS104/2_604; POS104/2_606; POS104/2_618; POS104/2_620; POS104/2_622; POS104/2_624; POS104/2_626; POS104/2_628; POS104/2_630; POS104/2_632; POS104/2_634; POS104/2_636; POS104/2_638; POS104/2_640; POS104/2_642; POS104/2_644; POS104/2_646; POS104/2_648; POS104/2_650; POS104/2_652; POS104/2_654; POS104/2_657; POS104/2_659; POS104/2_661; POS104/2_663; POS104/2_665; POS104/2_667; POS104/2_669; POS104/2_671; POS104/2_672; POS104/2_674; POS104/2_677; Poseidon; Pressure, water; Salinity; SFB133; South Atlantic Ocean; Temperature, water; Warmwassersphäre des Atlantiks
    Type: Dataset
    Format: text/tab-separated-values, 496784 data points
    Location Call Number Limitation Availability
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    DATA PANGAEA
  • 15
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    Unknown
    The response of drifting buoys to currents and wind (1989)
    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 94 (C3). pp. 3201-3210.
    Details
    Publication Date: 2020-10-20
    Description: Two buoy types have been tested with respect to their drift performance under drogued and undrogued conditions. Additionally, forces acting on the buoys were measured directly. Quadratic drag laws have been confirmed for the drag in water and the combined drag of wind and waves. Stokes drift contributes about one half to the wind factor of 0.023, which is obtained for undrogued buoys in the Atlantic. The forces on a windowshade drogue are given by a linear relation between force and water velocity for speeds exceeding 10 cm/s. They have been extrapolated to speeds of less than 10 cm/s by both a linear and a quadratic relationship. Correlations between drift and wind speed in the Atlantic suggest that the linear law is a better approximation under realistic conditions. According to these measurements in the Atlantic the described buoy-drogue system with a windowshade drogue in 100-m depth is a good current-measuring device. Slippage is negligible for wind speeds of less than 15 m/s and is less than 2 cm/s under gale conditions. Undrogued buoys are strongly affected by wind and cannot be used for the analysis of currents without correction, even under light winds.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1029/JC094iC03p03201
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 16
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    Lagrangian properties of eddy fields in the northern North Atlantic as deduced from satellite-tracked buoys (1987)
    Sears Foundation of Marine Research
    In:  Journal of Marine Research, 45 . pp. 259-291.
    Details
    Publication Date: 2018-01-24
    Description: One hundred and thirteen satellite-tracked buoys have been used during their first 5 months after deployment in order to calculate Lagrangian statistics of the eddy field in the northern North Atlantic between Newfoundland and the Canary basin. r.m.s. velocities are isotropic and increase from southeast to northwest. Lagrangian integral time scales, derived both from correlation function and from dispersion, are slightly anisotropic and decrease from the subtropics toward the North Atlantic Current. Time scale is inversely proportional to the r.m.s. velocity of the eddies. Eddy length scale is approximately constant in the North Atlantic. Dispersion is in good agreement with Taylor's hypothesis, following a t2-law during the first day after release and a linear increase with time during days 10 to 60. Eddy diffusivity increases from 30N to 50N by a factor of about 4 and is linearly dependent on the r.m.s. velocity. The energy containing frequency band of the eddies shifts toward higher frequencies in the northern part of the Atlantic. Beyond the cut-off frequency of the eddies the spectral slope follows a -2 or -3 power law.
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1357/002224087788401142
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    OceanRep: Article in a Scientific Journal - peer-reviewed
  • 17
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    Unknown
    Nordostatlantik '84 : Data Report (1985)
    Institut für Meereskunde
    In:  Berichte aus dem Institut für Meereskunde an der Christian-Albrechts-Universität Kiel, 146 . Institut für Meereskunde, Kiel, Germany, 80 pp.
    Details
    Publication Date: 2019-09-23
    Type: Report , NonPeerReviewed
    Format: text
    DOI: 10.3289/IFM_BER_146
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    OceanRep: Report - Data report
  • 18
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    Günter Dietrichs Kieler Jahre : 1959-1972 (1987)
    Wachholtz
    In:  Christiana Albertina, 24 (N.F.) . pp. 43-54.
    Details
    Publication Date: 2016-07-13
    Type: Article , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
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    OceanRep: Article in a Scientific Journal - without review
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