Impact of acoustic Doppler current profiler (ADCP) motion on structure function estimates of turbulent kinetic energy dissipation rate
-
Published:2022-02-03
Issue:1
Volume:18
Page:169-192
-
ISSN:1812-0792
-
Container-title:Ocean Science
-
language:en
-
Short-container-title:Ocean Sci.
Author:
Scannell Brian D.ORCID, Lenn Yueng-Djern, Rippeth Tom P.ORCID
Abstract
Abstract. Turbulent mixing is a key process in the transport of heat, salt, and nutrients in the marine environment, with fluxes commonly derived directly from estimates of the turbulent kinetic energy dissipation rate, ε. Time series of ε estimates are therefore useful in helping to identify and quantify key biogeochemical processes.
The velocity structure function method can be used to determine time series of ε estimates using along-beam velocity measurements from suitably configured acoustic Doppler current profilers (ADCPs). Shear in the background current can bias such estimates; therefore, standard practice is to deduct the mean or linear trend from the along-beam velocity over the period of an observation burst. This procedure is effective if the orientation of the ADCP to the current remains constant over the burst period. However, if the orientation of the ADCP varies, a proportion of the velocity difference between bins is retained in the structure function and the resulting ε estimates will be biased. Long-term observations from a mooring with three inline ADCPs show the heading oscillating with an angular range that depends on the flow speed: from large, slow oscillations at low flow speeds to smaller, higher-frequency oscillations at higher flow speeds. The mean tilt was also determined by the flow speed, whilst the tilt oscillation range was primarily determined by surface wave height. Synthesised along-beam velocity data for an ADCP subject to sinusoidal oscillation in a sheared flow indicate that the retained proportion of the potential bias is primarily determined by the angular range of the oscillation, with the impact varying between beams depending on the mean heading relative to the flow. Since the heading is typically unconstrained in a tethered mooring, heading oscillation is likely to be the most significant influence on the retained bias for a given level of shear. Use of an instrument housing designed to reduce oscillation would mitigate the impact, whilst if the shear is linear over the observation depth range, the bias can be corrected using a modified structure function method designed to correct for bias due to surface waves.
Funder
UK Research and Innovation
Publisher
Copernicus GmbH
Subject
Cell Biology,Developmental Biology,Embryology,Anatomy
Reference36 articles.
1. Bluteau, C. E., Jones, N. L., and Ivey, G. N.: Acquiring Long-Term Turbulence
Measurements from Moored Platforms Impacted by Motion, J.
Atmos. Ocean. Tech., 33, 2535–2551,
https://doi.org/10.1175/JTECH-D-16-0041.1, 2016. a 2. Buckingham, C. E., Lucas, N. S., Belcher, S. E., Rippeth, T. P., Grant, A.
L. M., Le Sommer, J., Ajayi, A. O., and Naveira Garabato, A. C.: The
Contribution of Surface and Submesoscale Processes to Turbulence in the Open
Ocean Surface Boundary Layer, J. Adv. Model. Earth Sy.,
11, 4066–4094, https://doi.org/10.1029/2019MS001801, 2019. a, b 3. Codiga, D. L.: Unified Tidal Analysis and Prediction Using the UTide Matlab
Functions, Technical Report 2011-01, Graduate School of Oceanography,
University of Rhode Island, Narragansett, RI, 2011. a 4. Dewey, R. K., Crawford, W. R., Gargett, A. E., and Oakey, N. S.: A
Microstructure Instrument for Profiling Oceanic Turbulence in Coastal Bottom
Boundary Layers, J. Atmos. Ocean. Tech., 4, 288–297,
https://doi.org/10.1175/1520-0426(1987)004<0288:AMIFPO>2.0.CO;2, 1987. a 5. Fer, I., Peterson, A. K., and Ullgren, J. E.: Microstructure Measurements from
an Underwater Glider in the Turbulent Faroe Bank Channel Overflow, J. Atmos. Ocean. Tech., 31, 1128–1150,
https://doi.org/10.1175/JTECH-D-13-00221.1, 2014. a
Cited by
3 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|