Fully Lagrangian Floats in Labrador Sea Deep Convection: Comparison of Numerical and Experimental Results
Authors:
- Ramsey R. HarcourtRHRamsey R. Harcourt
- Elizabeth L. SteffenESElizabeth L. Steffen
- Roland W. GarwoodRGRoland W. Garwood
- Eric A. D'AsaroEDEric A. D'Asaro
Open Access
- 1 February 2002
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 32 (2) , 493-510
Abstract
Measurements of deep convection from fully Lagrangian floats deployed in the Labrador Sea during February and March 1997 are compared with results from model drifters embedded in a large eddy simulation (LES) of the rapidly deepening mixed layer. The deep Lagrangian floats (DLFs) have a large vertical drag, and are designed to nearly match the density and compressibility of seawater. The high-resolution numerical simulation of deep convective turbulence uses initial conditions and surface forcing obtained from in situ oceanic and atmospheric observations made by the R/V Knorr. The response of model floats to the resolved large eddy fields of buoyancy and velocity is simulated for floats that are 5 g too buoyant, as well as for floats that are correctly ballasted. Mean profiles of potential temperature, Lagrangian rates of heating and acceleration, vertical turbulent kinetic energy (TKE), vertical heat flux, potential temperature variance, and float probability distribution functions (PDFs) are co... Abstract Measurements of deep convection from fully Lagrangian floats deployed in the Labrador Sea during February and March 1997 are compared with results from model drifters embedded in a large eddy simulation (LES) of the rapidly deepening mixed layer. The deep Lagrangian floats (DLFs) have a large vertical drag, and are designed to nearly match the density and compressibility of seawater. The high-resolution numerical simulation of deep convective turbulence uses initial conditions and surface forcing obtained from in situ oceanic and atmospheric observations made by the R/V Knorr. The response of model floats to the resolved large eddy fields of buoyancy and velocity is simulated for floats that are 5 g too buoyant, as well as for floats that are correctly ballasted. Mean profiles of potential temperature, Lagrangian rates of heating and acceleration, vertical turbulent kinetic energy (TKE), vertical heat flux, potential temperature variance, and float probability distribution functions (PDFs) are co...Keywords
This publication has 20 references indexed in Scilit:
- Temperature and Salinity Variability in Heterogeneous Oceanic Convection*Journal of Physical Oceanography, 2000
- The Labrador Sea Deep Convection ExperimentBulletin of the American Meteorological Society, 1998
- A Lagrangian FloatJournal of Atmospheric and Oceanic Technology, 1996
- An ocean large‐eddy simulation model with application to deep convection in the Greenland SeaJournal of Geophysical Research: Oceans, 1996
- Unsteady, Turbulent Convection into a Rotating, Linearly Stratified Fluid: Modeling Deep Ocean ConvectionJournal of Physical Oceanography, 1995
- The Formation of Labrador Sea Water. Part II. Mesoscale and Smaller-Scale ProcessesJournal of Physical Oceanography, 1983
- Oceanographic conditions at Ocean Weather ShipBravo, 1964–1974Atmosphere-Ocean, 1980
- The Use of Subgrid Transport Equations in a Three-Dimensional Model of Atmospheric TurbulenceJournal of Fluids Engineering, 1973
- The renewal of Labrador sea waterDeep Sea Research and Oceanographic Abstracts, 1973
- On the magnitude of the subgrid scale eddy coefficientJournal of Computational Physics, 1971