Zobrazeno 1 - 10
of 68
pro vyhledávání: '"Ann E. Gargett"'
Autor:
Ann E. Gargett, Dana K. Savidge
Publikováno v:
Journal of Physical Oceanography. 50:1341-1364
Measurements of collocated fields of atmospheric forcing, surface waves, and mean and turbulent velocities associated with passage of Tropical Storm (TS) Barry over the U.S. Navy Tower R2 on the Georgia continental shelf are presented. A vertical-bea
Autor:
Ann E. Gargett
Publikováno v:
Journal of Marine Research. 77:243-266
This study examines a simple 6-box model of a single pole-to-pole ocean basin. Each of a northern "polar gyre," a southern "polar gyre," and an "equatorial gyre," consisting of north and south subtropical gyres plus the equatorial region, is represen
Autor:
Ann E. Gargett
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 34:1387-1390
Greene et al. revisit the suggestion that the turbulent kinetic energy dissipation rate could be estimated through a “large-eddy estimate,” employing acoustic measurements of velocity fields associated with the largest energy-containing scales of
Autor:
Ann E. Gargett, Dana K. Savidge
Publikováno v:
Journal of Marine Research. 75:49-79
Autor:
Ann E. Gargett, Dana K. Savidge
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 33:1089-1095
With standard low-frequency velocity data from current meter moorings, pressure gradient–driven mean flow is determined by low-pass filtering, while tides are estimated by fitting tidal constituents, with accuracy and numbers of constituents determ
Autor:
Chester E. Grosch, Ann E. Gargett
Publikováno v:
Journal of Physical Oceanography. 46:3595-3597
Existing large-eddy simulations (LES) of Langmuir supercells (LS) do not include rotational terms. Despite the fact that the actual coastal ocean is certainly affected by rotation, such simulations are found to provide excellent agreement with a wide
Publikováno v:
Journal of Marine Research. 72:127-163
Autor:
Chester E. Grosch, Ann E. Gargett
Publikováno v:
Journal of Physical Oceanography. 44:44-67
Turbulence in the ocean surface layer is generated by time-varying combinations of destabilizing surface buoyancy flux, wind stress forcing, and wave forcing through a vortex force associated with the surface wave field. Observations of time- and dep
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 63:118-132
Detailed studies were made in the springtime Ross Sea Polynya of the interaction between near-surface mixing processes, inferred from Thorpe scales and acoustic backscatter, and the quantum efficiency and rate of PSII electron transport of phytoplank