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Repeated temperature profiles were obtained at a slowly sinking and rising free float in a depth range of 1300 to 3600 m at 10°24′N, 50°22′W during the period 15–17 October 1967. Temperature deviation...
Measurements of Wind-Driven Flow Profiles in the Top Millimeter of Water
Wind-Driven Flow Profiles Top Millimeter
2009/3/24
Shapes of mean water velocity profiles measured with microscopic bubble tracers in developing, laminar flows are recognizably different from those in a turbulent flow. A previously deduced viscous sub...
A method is developed for the computation of dynamic height from temperature data alone by using a mean T-S relationship to provide salinity values. This method is tested at three Pacific weathership ...
A Study of Velocity Profiles Through the Main Thermocline
Velocity Profiles Main Thermocline
2009/3/7
A time series of velocity profiles derived from three methods are used to describe the variations of current in time and in the vertical. Absolute velocity profiles were Obtained by acoustically track...
Simultaneous Current-Temperature Profiles in the Equatorial Counter Current
Global Atmospheric Research Program Atlantic Tropical Experiment Simultaneous Current-Temperature Profiles
2009/3/7
Serial current and temperature measurements were made during the Global Atmospheric Research Program Atlantic Tropical Experiment (GATE) with unattended autonomous profilers (Cyclesondes) in the North...
On Wind-Driven Current and Temperature Profiles with Diurnal Period in the Oceanic Planetary Boundary Layer
Wind-Driven Current Diurnal Period Temperature Profiles
2009/2/13
This paper describes a physically reliable model of the ocean surface layer. A Richardson-number-dependent stability function obtained from atmospheric boundary-layer data is applied to the oceanic la...
The Effects of Bias Error and System Noise on Parameters Computed from C, T, P and V Profiles
Bias Error V Profiles System Noise
2009/2/11
The development of high-resolution profiling instruments has made possible the computation of quantities such as the stability parameter N2 and the Richardson number Ri over scales of less than a mete...
Richardson Number Profiles over the Continental Shelf
Continental Shelf Richardson Number Profiles
2009/2/6
The seasonal mid-water thermocline over the continental shelf has been examined with the aid of an oceanographic Richardson Number Probe. The overall Richardson number of this stable layer was found t...
Equatorial Velocity Profiles. Part II：Zonal Component
Zonal Component Equatorial Velocity Profiles
2009/1/21
Vertical profiles of horizontal velocity made along 53°E in the western Indian Ocean, during and after he onset of the southwest monsoon in 1976, show features in zonal velocity of relatively small ve...
Equatorial Velocity Profiles. Part I：Meridional Component
dropped lagged coherence Equatorial Velocity Profiles Meridional Component
2009/1/21
A time series or vertical profiles of horizontal velocity was collected in the western equatorial Indian Ocean during late spring of 1976. The meridional velocity component is examined here, the zonal...
The Subthermocline Lens D1. Part I：Description of Water Properties and Velocity Profiles
Local Dynamics Experiment Water Properties Velocity Profiles
2009/1/10
One remarkable result of the Local Dynamics Experiment in POLYMODE is the discovery of a large number of small energetic eddies. Using CTD data, SOFAR float tracks, and profiles of absolute velocity, ...
Bottom Stress Estimates from Vertical Dissipation Rate Profiles on the Continental Shelf
Bottom Stress Continental Shelf Vertical Dissipation Rate Profiles
2009/1/6
Measurements of the near-bottom distribution of the turbulent dissipation rate on the continental shelf west of Vancouver Island are used to calculate bottom stress. A free-failing vertical profiler w...
Statistics of Shear and Turbulent Dissipation Profiles in Random Internal Wave Fields
Turbulent Dissipation Profiles Random Internal Wave Fields
2008/12/19
Because breaking internal waves produces most of the turbulence in the thermocline, the statistics of , the rate of turbulent dissipation, cannot be understood apart from the statistics of internal wa...
On the Linear Approximation of Velocity and Density Profiles in the Problem of Baroclinic Instability
Linear Approximation Density Profiles Baroclinic Instability
2008/7/11
The linear approximation of density and velocity profiles is compared to more realistic models with vertically inhomogeneous density gradients and nonzero anomalous vorticity (i.e., the nonplanetary p...
Modeling Tidal Current Profiles and Vertical Mixing beneath Filchner–Ronne Ice Shelf, Antarctica（图）
Modeling Tidal Current Vertical Mixing Filchner–Ronne Ice Shelf Antarctica
2008/5/28
One of the warmest water masses beneath Filchner–Ronne Ice Shelf (FRIS) is dense, high salinity shelf water (HSSW) that flows into the sub-ice-shelf cavity from the ice front and occupies the lower po...