Cited by 47Oceanographic and Atmospheric ProcessesFluid Dynamics and Turbulent FlowsOcean Waves and Remote Sensing

Comparison of Thermal Variance Dissipation Rates from Moored and Profiling Instruments at the Equator

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Perlin, A., Moum, J. N.·2012·Journal of Atmospheric and Oceanic Technology

Abstract

As a quantitative test of moored mixing measurements using χpods, a comparison experiment was conducted at 0°, 140°W in October–November 2008. The following three measurement elements were involved: (i) NOAA’s Tropical Atmosphere Ocean (TAO) mooring with five χpods, (ii) a similar mooring 9 km away with seven χpods, and (iii) Chameleon turbulence profiles at an intermediate location. Dissipation rates of temperature variance and turbulent kinetic energy are compared. In all but 3 of 17 direct comparisons 15-day mean values of χT agreed within 95% bootstrap confidence limits computed with the conservative assumption that individual 1-min χpod averages and individual Chameleon profiles are independent. However, significant mean differences occur on 2-day averages. Averaging in time reduces the range (95%) in the observed differences at two locations from a factor of 17 at 1-day averaging time to less than a factor of 2 at 15 days, presumably reflecting the natural variability in both the turbulence and the small-scale fluid dynamics that lead to instability and turbulence. The motion of χpod on a mooring beneath a surface buoy is complex and requires a complete motion package to define in detail. However, perfect knowledge of the motion of the sensor tip is not necessary to obtain a reasonable measure of χT. A sampling test indicated that the most important motion sensor is a pressure sensor sampled rapidly enough to resolve the surface wave–induced motion.

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  • Confidence in these measurements is justified by previous comparisons between 16-day averages of ε from shipboard profiling (using shear probes) and multiple χpods on both the TAO mooring and an additional nearby mooring that showed agreement to within a factor of 2.

    “Confidence in these measurements is justified by previous comparisons between 16-day averages of ϵ from (i) shipboard profiling (using shear probes) and (ii) multiple χpods on both the TAO mooring and an additional nearby mooring that showed agreement to within a factor of 2 (Perlin & Moum, 2012).”

    From Deep Cycle Turbulence in Atlantic and Pacific Cold Tongues (2022) · cites this paper as Perlin & Moum, 2012

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Research works printed but not linked: 3

  1. --, R.-C. Lien, A. Perlin, J. D. Nash, M. C. Gregg, and P. J. Wiles, 2009: Sea surface cooling at the equator by subsurface mix- ing in tropical instability waves. Nat. Geosci., 2, 761-765, doi:10.1038/NGEO657. · DOI · Paper page
  2. Walchko, K. J., 2002: Low cost inertial navigation: Learning to integrate noise and find your way. M.S. thesis, Dept. of Electrical and Computer Engineering, University of Florida, 80 pp. [Available online at http://www.mil.ufl.edu/publica- tions/thes_diss/Kevin_Walchko_thesis.pdf.
  3. Wiles, P. J., T. P. Rippeth, J. H. Simpson, and P. J. Hendricks, 2006: A novel technique for measuring the rate of turbulence dis- sipation in the marine environment. Geophys. Res. Let., 33, L21608, doi:10.1029/2006GL027050. · DOI

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  • Deep Cycle Turbulence in Atlantic and Pacific Cold Tongues

    Moum, J. N., Hughes, K. G., Shroyer, E. L., Smyth, W. D., Cherian, D., Warner, S. J., Bourlès, B., Brandt, P., & Dengler, M. (2022) · Geophysical Research Letters · doi:10.1029/2021gl097345 · Cited by 34 · see citing works

    “Moored turbulence measurements using χpods (Moum & Nash, 2009) have time resolution sufficient to resolve property (2) and now also extend over many years at a few sites.”
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Authors
Perlin, A., & Moum, J. N.
Affiliations
Oregon State University (US)
Corresponding author
Perlin, A.
Venue
Journal of Atmospheric and Oceanic Technology
Published
2012-09-01
Volume
29
Issue
9
Pages
1347-1362
ISSN
  • 0739-0572 (ISSN-L)
  • 1520-0426
OpenAlex
W2132297963
Cited by
47
References
0
Citations by year
2025: 1 · 2024: 2 · 2023: 3 · 2022: 5 · 2021: 5 · 2020: 4 · 2019: 5 · 2018: 1 · 2017: 7 · 2016: 7 · 2015: 2 · 2014: 1 · 2013: 3 · 2012: 1
FWCI
1.66
Type
journal article
Language
en
Open access
Locations
Journal of Atmospheric and Oceanic Technology (publishedVersion)
Funders
  • National Science Foundation (0728375)
  • University of Washington
  • National Oceanic and Atmospheric Administration
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Engineering › Computational Mechanics › Fluid Dynamics and Turbulent Flows
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Waves and Remote Sensing
Keywords
turbulent kinetic energy dissipation, equatorial ocean, sensor motion

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