Correcting surface wave bias in structure function estimates of turbulent kinetic energy dissipation rate
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
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Yn: Journal of Atmospheric and Oceanic Technology, Cyfrol 34, Rhif 10, 10.2017, t. 2257-2273.
Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid
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T1 - Correcting surface wave bias in structure function estimates of turbulent kinetic energy dissipation rate
AU - Scannell, Brian
AU - Rippeth, Thomas
AU - Simpson, John
AU - Polton, Jeff
AU - Hopkins, Jo
N1 - Brian Scannell is an ENVISION DTP PhD student
PY - 2017/10
Y1 - 2017/10
N2 - The combination of acoustic Doppler current profilers and the structurefunction methodology provide an attractive approach to making extended timeseries measurements of oceanic turbulence (the rate of turbulent kinetic energydissipation, e) from moorings. However, we show that for deploymentsin the upper part of the water column, estimates of e will be biased by thevertical gradient in wave orbital velocities. To remove this bias, we develop amodified structure function methodology, which exploits the differing lengthscale dependencies of the contributions to the structure function due to turbulent and wave orbital motions. The success of the modified method is demonstrated through comparison of e estimates based on data from instruments at three depths over a three month period under a wide range of conditions, with appropriate scalings for wind stress and convective forcing.
AB - The combination of acoustic Doppler current profilers and the structurefunction methodology provide an attractive approach to making extended timeseries measurements of oceanic turbulence (the rate of turbulent kinetic energydissipation, e) from moorings. However, we show that for deploymentsin the upper part of the water column, estimates of e will be biased by thevertical gradient in wave orbital velocities. To remove this bias, we develop amodified structure function methodology, which exploits the differing lengthscale dependencies of the contributions to the structure function due to turbulent and wave orbital motions. The success of the modified method is demonstrated through comparison of e estimates based on data from instruments at three depths over a three month period under a wide range of conditions, with appropriate scalings for wind stress and convective forcing.
KW - OCEANOGRAPHY
U2 - 10.1175/JTECH-D-17-0059.1
DO - 10.1175/JTECH-D-17-0059.1
M3 - Article
VL - 34
SP - 2257
EP - 2273
JO - Journal of Atmospheric and Oceanic Technology
JF - Journal of Atmospheric and Oceanic Technology
SN - 0739-0572
IS - 10
ER -