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  • Matlab  (6)
  • Ocean-atmosphere interaction  (2)
  • Wind forcing  (2)
  • 1
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    Unknown
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2015. This is the author's version of the work. It is posted here by permission of Annual Reviews for personal use, not for redistribution. The definitive version was published in Annual Review of Marine Science 8 (2016): 59-78, doi:10.1146/annurev-marine-010814-015717.
    Description: Cross-shelf exchange dominates the pathways and rates by which nutrients, biota and materials on the continental shelf are delivered and removed. These transports are limited by Earth’s rotation, which inhibits flow from crossing isobaths. Thus, cross-shelf transports are generally weak compared to alongshore flows, and this leads to interesting observational issues. Cross-shelf flows are enabled by turbulent mixing processes, by nonlinear processes (such as momentum advection), and by time-dependence. Thus, there is a wide range of possible effects that can allow these critical transports, and different natural settings are often governed by differing mixes of processes. Examples of representative transport mechanisms are discussed, and possible observational and theoretical paths to future progress are explored.
    Description: Support from the National Science Foundation Physical Oceanography program, through grant OCE-1433953, and the Biological Oceanography program through grant OCE-1258667
    Keywords: Coastal physical oceanography ; Turbulent boundary layers ; Coastal instabilities ; Nutrient supplies ; Wind forcing
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 2
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    Unknown
    Sears Foundation for Marine Research
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author, 2018. This article is posted here by permission of [publisher] for personal use, not for redistribution. The definitive version was published in Journal of Marine Research 76 (2018): 1-22, doi:10.1357/002224018824082016.
    Description: An idealized numerical model is used to explore the generation of mean flows by oscillating wind forcing in a stratified coastal ocean with no alongshore variability, i.e., where neither barotropic nor baroclinic instability is a factor. On the inner shelf, where surface-to-bottom mixing occurs, a mean cross-shelf flow develops, as examined by Castelao et al. (2010), and the present results suggest that this flow can remain two-dimensional if there is a nonzero cross-shelf density gradient. Offshore of the inner shelf, where the water column is stratified, a mean alongshore flow develops in the direction opposite to coastal-trapped wave propagation. This flow is associated with cross-shelf density gradients that are set up by the asymmetry between onshore and offshore flow in the bottom boundary layer. Both forms of rectified flow (cross-shelf and alongshore) are sensitive to the presence of surface heating, and the rectifications can be readily masked by the effect of a steady alongshore wind stress.
    Description: This research was partially supported by the National Science Foundation Physical Oceanography Program through grant OCE-1433953.
    Keywords: Continental shelf ; Rectified flow ; Wind forcing
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 3
    Publication Date: 2022-05-26
    Description: Frontal Air-Sea Interaction Experiment (FASINEX) contribution no. 46
    Description: The Frontal Air-Sea Interaction Experiment (FASINEX) examined air-sea interaction in the vicinity of sea surface temperature fronts in the Subtropical Convergence Zone (STCZ). Mooring measurements were made from five surface, four Profiling Current Meter (PCM) and two longer duration subsurface moorings. The surface and PCM moorings, which made up the FASINEX central array were set in January 1986 and remained on station for six months. The two outlying subsurface moorings, set 90 miles south and 30 miles north of the central array were deployed in October 1984 and were recovered with the central array moorings in June 1986. The surface moorings collected oceanographic and meteorological data, using a 3-meter instrumented discus buoy and eight to ten Vector Measuring Current Meters (VMCMs) and Vector Averaging Current Meters (VACMs). The surface buoy carried a Vector Measuring Wind recorder (VAWR) and a Meteorological Recorder (MR) which measured wind speed and direction, sea surface temperature (SST), air temperature, insolation, barometric pressure and relative humidity. The MR also transmitted meteorological and engineering data via ARGOS. The VMCMs and VACMs, placed from 10 to 4000 m, measured oceanic velocities and temperatures. The subsurface moorings measured oceanic velocities and temperature from 160 to 4060 m, carrying a total of seven VACMs and a WOTAN (Wind Observations Through Ambient Noise). This report presents meteorological and oceanographic data from the seven W.H.O.I. moorings, with major emphasis on the surface mooring data. Details of the moored array and a statement of data return and quality are also included.
    Description: Funding was provided by the Office of Naval Research under contract Number N00014-84-C-0134.
    Keywords: Ocean-atmosphere interaction ; Endeavor (Ship: 1976-) Cruise ; Oceanus (Ship : 1975-) Cruise ; Knorr (Ship : 1970-) Cruise ; Columbus Iselin (Ship) Cruise
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: application/pdf
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  • 4
    Publication Date: 2022-05-26
    Description: The OPUS (Organization of Persistent Upwelling Structures) program deployed two current meter (VMCM) moorings near Point Conception, California, during April-July 1983. Current and temperature data from these moorings are summarized here. In addition, data from two nearby NDBC (National Data Buoy Center) meteorological buoys are presented.
    Description: Funding was provided by the National Science Foundation under grants OCE 82-13968 and OCE 80-14942.
    Keywords: Upwelling ; Ocean currents ; Ocean-atmosphere interaction
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 5
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    Unknown
    Woods Hole Oceanographic Institution
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all with names beginning with “bwavesp”) can be used to calculate barotropic coastal wave properties in the absence of density stratification. The wave frequency is taken to be entirely real (hence stable). You are allowed to have a mean alongshore flow, if desired, and you can apply the rigid lid and/or coastal long wave approximations. The model can be run in the non-rotating limit if desired. Once a wave’s frequency is found, the modal structure is displayed, and a perturbation (weak friction) imaginary correction to the wave frequency is found. The code can use an exact open boundary condition or a closed condition at either side of the domain.
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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  • 6
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all having names that begin with “bigs”) can be used to calculate seamount-trapped (or basin-trapped) wave modal structures and dispersion curves under very general circumstances. A complex frequency is allowed, so that instability and damping can be accounted for directly. Modal structures and energy diagnostics are provided. For most applications, the code is only useful for subinertial wave frequencies (i.e., the real part of wave frequency is smaller than the Coriolis parameter). For interpreting the model results, see Brink (1989), which deals with the case with no mean flow or finite bottom friction. The present code was developed independently of the Fortran code used in that publication.
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Software
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  • 7
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all having names that begin with “bigi”) can be used to calculate island-trapped wave modal structures and dispersion curves under very general circumstances for a circular island. A complex frequency is allowed, so that instability and damping can be accounted for directly. Modal structures and energy diagnostics are provided. For most applications, the code is only useful for subinertial wave frequencies (i.e., the real part of wave frequency is smaller than the Coriolis parameter). For interpreting the model results, see Brink (1999), which deals with the case with no mean flow or finite bottom friction. The present code was developed independently of the Fortran code used in that publication.
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Software
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all having names that begin with “bigr”) can be used to calculate stable, inviscid coastal-trapped wave modal structures and dispersion curves under very general circumstances. Only a real frequency is allowed, so that instability and damping cannot be accounted for directly, but computations are more efficient than for the general case, long-wave parameters can be computed for first order wave equation calculations (see Brink, 1989), and a more general perturbation decay time (Brink, 1990) can also be obtained. Modal structures and energy diagnostics are provided. Generally speaking, the code is only useful for subinertial wave frequencies.
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Software
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all having names that begin with “bigc”) can be used to calculate coastal-trapped wave modal structures and dispersion curves under very general circumstances. A complex frequency is allowed, so that instability and damping can be accounted for directly. Modal structures and energy diagnostics are provided. For most applications, the code is only useful for subinertial wave frequencies (i.e., the real part of wave frequency is smaller than the Coriolis parameter).
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Software
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2022-10-21
    Description: This set of Matlab mfiles (all with names beginning with “bwavesc”) can be used to calculate barotropic coastal wave properties in the absence of density stratification. The wave frequency is complex so that unstable or strongly damped modes can be treated. You are allowed to have a mean alongshore flow, if desired, and you can apply the rigid lid approximation. The model can be run in the non-rotating limit if desired. Once a wave’s frequency is found, the modal structure is displayed. The code can use an exact open boundary condition or a closed condition at either side of the domain.
    Keywords: Matlab ; Wave modal structures ; Dispersion curves
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
    Location Call Number Limitation Availability
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