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  • 1
    Online-Ressource
    Online-Ressource
    American Meteorological Society ; 2007
    In:  Bulletin of the American Meteorological Society Vol. 88, No. 3 ( 2007-03-01), p. 341-356
    In: Bulletin of the American Meteorological Society, American Meteorological Society, Vol. 88, No. 3 ( 2007-03-01), p. 341-356
    Kurzfassung: The Office of Naval Research's Coupled Boundary Layers and Air–Sea Transfer (CBLAST) program is being conducted to investigate the processes that couple the marine boundary layers and govern the exchange of heat, mass, and momentum across the air–sea interface. CBLAST-LOW was designed to investigate these processes at the low-wind extreme where the processes are often driven or strongly modulated by buoyant forcing. The focus was on conditions ranging from negligible wind stress, where buoyant forcing dominates, up to wind speeds where wave breaking and Langmuir circulations play a significant role in the exchange processes. The field program provided observations from a suite of platforms deployed in the coastal ocean south of Martha's Vineyard. Highlights from the measurement campaigns include direct measurement of the momentum and heat fluxes on both sides of the air–sea interface using a specially constructed Air–Sea Interaction Tower (ASIT), and quantification of regional oceanic variability over scales of O(1–104 mm) using a mesoscale mooring array, aircraft-borne remote sensors, drifters, and ship surveys. To our knowledge, the former represents the first successful attempt to directly and simultaneously measure the heat and momentum exchange on both sides of the air–sea interface. The latter provided a 3D picture of the oceanic boundary layer during the month-long main experiment. These observations have been combined with numerical models and direct numerical and large-eddy simulations to investigate the processes that couple the atmosphere and ocean under these conditions. For example, the oceanic measurements have been used in the Regional Ocean Modeling System (ROMS) to investigate the 3D evolution of regional ocean thermal stratification. The ultimate goal of these investigations is to incorporate improved parameterizations of these processes in coupled models such as the Coupled Ocean–Atmosphere Mesoscale Prediction System (COAMPS) to improve marine forecasts of wind, waves, and currents.
    Materialart: Online-Ressource
    ISSN: 0003-0007 , 1520-0477
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2007
    ZDB Id: 2029396-3
    ZDB Id: 419957-1
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
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    American Meteorological Society ; 2008
    In:  Journal of Physical Oceanography Vol. 38, No. 5 ( 2008-05-01), p. 1054-1072
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 38, No. 5 ( 2008-05-01), p. 1054-1072
    Kurzfassung: This study makes direct measurements of turbulent fluxes in the mixed layer in order to close heat and momentum budgets across the air–sea interface and to assess the ability of rigid-boundary turbulence models to predict mean vertical gradients beneath the ocean’s wavy surface. Observations were made at 20 Hz at nominal depths of 2.2 and 1.7 m in ∼16 m of water. A new method is developed to estimate the fluxes and the length scales of dominant flux-carrying eddies from cospectra at frequencies below the wave band. The results are compared to independent estimates of those quantities, with good agreement between the two sets of estimates. The observed temperature gradients were smaller than predicted by standard rigid-boundary closure models, consistent with the suggestion that wave breaking and Langmuir circulation increase turbulent diffusivity in the upper ocean. Similarly, the Monin–Obukhov stability function ϕh was smaller in the authors’ measurements than the stability functions used in rigid-boundary applications of the Monin–Obukhov similarity theory. The dominant horizontal length scales of flux-carrying turbulent eddies were found to be consistent with observations in the bottom boundary layer of the atmosphere and from laboratory experiments in three ways: 1) in statically unstable conditions, the eddy sizes scaled linearly with distance to the boundary; 2) in statically stable conditions, length scales decreased with increasing downward buoyancy flux; and 3) downwind length scales were larger than crosswind length scales.
    Materialart: Online-Ressource
    ISSN: 1520-0485 , 0022-3670
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2008
    ZDB Id: 2042184-9
    ZDB Id: 184162-2
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
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    American Geophysical Union (AGU) ; 2023
    In:  Geophysical Research Letters Vol. 50, No. 10 ( 2023-05-28)
    In: Geophysical Research Letters, American Geophysical Union (AGU), Vol. 50, No. 10 ( 2023-05-28)
    Kurzfassung: Based on observations and large eddy simulation (LES), we examine diurnal warm layer (DWL) depths for moderate wind conditions with swell Based on LES results, we develop a unified scaling for the minimum DWL depth considering shear and wave‐driven Langmuir turbulence (LT) Observed DWL depths are consistent with LES results that include LT indicating the importance of wave‐driven turbulence on DWL dynamics
    Materialart: Online-Ressource
    ISSN: 0094-8276 , 1944-8007
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2023
    ZDB Id: 2021599-X
    ZDB Id: 7403-2
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
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    American Geophysical Union (AGU) ; 1992
    In:  Journal of Geophysical Research: Oceans Vol. 97, No. C8 ( 1992-08-15), p. 12619-12638
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 97, No. C8 ( 1992-08-15), p. 12619-12638
    Kurzfassung: A free‐drifting buoy serving as an ice anchor and flotation sphere for a 125‐m instrumented mooring line was deployed in the Arctic pack ice by the R/V Polarstern in August 1987 at the northernmost point achieved by the Arktis IV expedition. Current measurements were made from this Arctic environmental drifting buoy (AEDB) using a 150‐kHz acoustic Doppler current profiler (ADCP) attached to the mooring line at a depth of 16 m below the flotation sphere with the transducers facing downward. Velocity profiles spanning depths between 35 and 327 m with 15‐m resolution were collected at half‐hour intervals over a period of 216 days while the buoy drifted from its starting point near 86°N, 22°E to about 70°N, 16°W. The full experimental record was separated into three sections corresponding to periods of the drift spent in the Nansen Basin, over the Yermak Plateau, and in the Greenland Sea. Velocity time series and spectra were computed, and results for the three analysis sections were compared. Spectra in the Nansen Basin were found to have energy levels significantly less than those typical for mid‐latitudes, roughly one third of the canonical Garrett‐Munk (GM) level, and a spectral slope between ƒ and 2.5ƒ that was significantly flatter than that expected from the GM model. Between 83°N and 81°N, as the buoy passed over the Yermak Plateau, internal wave energy increased to levels comparable to GM. Isolated, energetic near‐inertial wave packets with upward group velocity were observed in this portion of the record, presumably generated by interaction of the barotropic tide with the bottom topography of the plateau. Estimates of the upward energy flux from these near‐inertial packets were comparable to the downward fluxes from typical surface sources. Interpretation of the Greenland Sea section was complicated by ADCP sampling problems and a lack of Argos fixes, but the available data showed internal wave spectral levels that were intermediate between those of the Nansen Basin and Yermak Plateau and no evidence of upward‐propagating near‐inertial energy.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1992
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
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    Elsevier BV ; 2013
    In:  Deep Sea Research Part II: Topical Studies in Oceanography Vol. 91 ( 2013-7), p. 71-83
    In: Deep Sea Research Part II: Topical Studies in Oceanography, Elsevier BV, Vol. 91 ( 2013-7), p. 71-83
    Materialart: Online-Ressource
    ISSN: 0967-0645
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2013
    ZDB Id: 1141627-0
    ZDB Id: 1500312-7
    SSG: 14
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
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    American Meteorological Society ; 2010
    In:  Journal of Physical Oceanography Vol. 40, No. 8 ( 2010-08-01), p. 1910-1914
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 40, No. 8 ( 2010-08-01), p. 1910-1914
    Materialart: Online-Ressource
    ISSN: 1520-0485 , 0022-3670
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 2010
    ZDB Id: 2042184-9
    ZDB Id: 184162-2
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
    Online-Ressource
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    American Meteorological Society ; 1991
    In:  Journal of Atmospheric and Oceanic Technology Vol. 8, No. 1 ( 1991-02), p. 172-178
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 8, No. 1 ( 1991-02), p. 172-178
    Materialart: Online-Ressource
    ISSN: 0739-0572 , 1520-0426
    Sprache: Englisch
    Verlag: American Meteorological Society
    Publikationsdatum: 1991
    ZDB Id: 2021720-1
    ZDB Id: 48441-6
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
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    American Geophysical Union (AGU) ; 2022
    In:  Journal of Geophysical Research: Oceans Vol. 127, No. 5 ( 2022-05)
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 127, No. 5 ( 2022-05)
    Kurzfassung: Oblique offshore winds drive strong wind and wave misalignment due to longer along‐shore but limited offshore wind fetches Coherent Langmuir turbulence characteristics are predominantly observed under conditions of developed and wind‐aligned waves Large eddy simulations agree well with observed Langmuir turbulence characteristics in a fetch‐limited coastal ocean
    Materialart: Online-Ressource
    ISSN: 2169-9275 , 2169-9291
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 2022
    ZDB Id: 2016804-4
    ZDB Id: 161667-5
    ZDB Id: 3094219-6
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
    Online-Ressource
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    American Geophysical Union (AGU) ; 1995
    In:  Journal of Geophysical Research: Oceans Vol. 100, No. C4 ( 1995-04-15), p. 6605-6619
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 100, No. C4 ( 1995-04-15), p. 6605-6619
    Kurzfassung: The Marine Light‐Mixed Layers (MLML) experiments took place in the subarctic North Atlantic Ocean, approximately 275 miles south of Reykjavik, Iceland, during 1989 and 1991. The 1991 field program took place from April 30 to September 6 and included a central surface mooring to document the temporal evolution of physical, biological, and optical properties. In this paper we describe the physical variability observed at the 1991 mooring site, concentrating on the vertical structure of temperature and velocity in the upper 300 m of the water column and their changes in response to heat and momentum fluxes at the sea surface. The deployment period included the spring transition, when upper ocean re stratification was initiated after deep winter mixing, and the fall transition, when mixed layer deepening began again. The dominant signal in temperature was seasonal variation, with a 6°C increase observed at the sea surface from May to August. Prior to development of the seasonal stratification, a period dominated by near‐surface temperature variability was observed in association with a 15‐day mean flux of only 20 W m −2 into the ocean. Pronounced day/night oscillations of heat flux during this period resulted in alternating development and destruction of stratification and intense diurnal cycling of the mixed layer depth. A qualitative comparison of the observed temperature structure to the prediction of a one‐dimensional mixed layer model showed that local processes dominated during the initiation of restratification and during most of the summer warming period. Nonlocal processes were important after the fall transition.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1995
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
    Online-Ressource
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    American Geophysical Union (AGU) ; 1998
    In:  Journal of Geophysical Research: Oceans Vol. 103, No. C5 ( 1998-05-15), p. 10253-10272
    In: Journal of Geophysical Research: Oceans, American Geophysical Union (AGU), Vol. 103, No. C5 ( 1998-05-15), p. 10253-10272
    Kurzfassung: The semidiurnal tide within a 100 km square region of the western equatorial Pacific centered at 1.8° S, 156.1° E is examined using shipboard survey and mooring data collected during the Tropical Ocean Global Atmosphere Coupled Ocean‐Atmosphere Response Experiment (TOGA COARE). Baroclinic and barotropic tidal amplitudes and phases are estimated from the survey and mooring observations in the upper 300 m of the 1800 m deep ocean by specifying their horizontal and vertical structures. The barotropic tide is assumed to have zero horizontal wavenumber over the domain, while a component of the baroclinic tide that is phase‐locked to the barotropic tide is determined by a searching method using plane wave fits to the data. The estimated barotropic tidal current is in good agreement with tide models derived from TOPEX/POSEIDON observations. The plane wave analysis indicates a dominant mode one baroclinic wave propagating toward the northeast. The second vertical mode can also be detected. Given the phase differences between the M2 and S2 constituents in the barotropic and baroclinic tides, the source of the baroclinic tidal signal is determined to be about 320 km southwest of the observing region, at a series of islands and shallow ridges. The combined estimates of the barotropic and baroclinic tides typically account for only 40–60% of the observed semidiurnal band current variance in the mooring data, indicating the high degree of temporal and spatial variability of the baroclinic tide in this region. The results of this study suggest, however, that coherent barotropic and baroclinic tidal signals can be successfully distinguished in the deep ocean using shipboard survey data, even when the data are limited to the upper 300 m.
    Materialart: Online-Ressource
    ISSN: 0148-0227
    Sprache: Englisch
    Verlag: American Geophysical Union (AGU)
    Publikationsdatum: 1998
    ZDB Id: 2033040-6
    ZDB Id: 3094104-0
    ZDB Id: 2130824-X
    ZDB Id: 2016813-5
    ZDB Id: 2016810-X
    ZDB Id: 2403298-0
    ZDB Id: 2016800-7
    ZDB Id: 161666-3
    ZDB Id: 161667-5
    ZDB Id: 2969341-X
    ZDB Id: 161665-1
    ZDB Id: 3094268-8
    ZDB Id: 710256-2
    ZDB Id: 2016804-4
    ZDB Id: 3094181-7
    ZDB Id: 3094219-6
    ZDB Id: 3094167-2
    ZDB Id: 2220777-6
    ZDB Id: 3094197-0
    SSG: 16,13
    Standort Signatur Einschränkungen Verfügbarkeit
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