We have contrived a model E(αω) α μ−1ω−p+1(ω 2−ω i 2)−+ for the distribution of internal wave energy in horizontal wavenumber, frequency-space, with wavenumber α extending to some upper limit μ(ω) α ω r-1 (ω 2−ω i 2)½, and frequency ω extending from the inertial frequency ω i to the local Väisälä frequency n(y). The…
Geophysical Fluid Dynamics Template
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About the Geophysical Fluid Dynamics format
Geophysical Fluid Dynamics is a peer-reviewed journal published by Taylor & Francis, covering Oceanographic and Atmospheric Processes, Ocean Waves and Remote Sensing, Fluid Dynamics and Turbulent Flows.
| Publisher | Taylor & Francis |
|---|---|
| Reference style | Author–year (Chicago, T&F) Author–year — (Smith, 2023) in the text Smith, Ada, Ben Jones, and Cara Lee. 2023. "A Representative Article Title." Geophysical Fluid Dynamics 12 (3): 45–58.
Formats any DOI in Geophysical Fluid Dynamics style. No sign-up. |
| Publishes research in | Oceanographic and Atmospheric Processes Ocean Waves and Remote Sensing Fluid Dynamics and Turbulent Flows Solar and Space Plasma Dynamics Geomagnetism and Paleomagnetism Studies |
| ISSN | 0016-7991 |
| h-index | 40 |
| i10-index | 89 |
| Total citations | 7,612 |
| Top institutions publishing here | NOAA Geophysical Fluid Dynamics Laboratory |
| Journal website | www.tandfonline.com |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Papers published in Geophysical Fluid Dynamics per year
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Most-cited papers in Geophysical Fluid Dynamics
AbstractA simple model is given that describes the response of the upper ocean to an imposed wind stress. The stress drives both mean and turbulent flow near the surface, which is taken to mix thoroughly a layer of depth h, and to erode the stably stratified fluid below. A marginal stability criterion based on a…
Measurements by free fall instruments, in the San Diego Trough, the Florida Current, and the central Pacific, reveal the detailed structure of the vertical component of the oceanic temperature gradient. The temperature changes are concentrated into regions on the order of a meter thick wherein the measured gradients are often more than ten times the…
Abstract It is found that in a rotating stratified fluid bounded by a single rigid wall, edge waves may occur at all frequencies less than or equal to N sin a (a is the angle of the wall from the horizontal and N the Brunt‐Vaisala frequency). These decay exponentially away from the boundary, in a…
Several effects of a baroclinic current on inertial‐internal waves at constant frequency are investigated, primarily through use of the method of characteristics. The special case of waves propagating transverse to a baroclinic current is considered. When the slope of an isopycnal is of the same order of magnitude as the slope of the characteristics, appreciable…