Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs

The calculation of the turbulent stress matrix using acoustic Doppler current profiler (ADCP) data remains a challenging problem in the study of geophysical flows. One of the ways to overcome the problem is to use a system of two coupled ADCP with pairs of beams intersecting at a certain depth. When...

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Main Authors: Sergey Bogdanov, Igor Maksimov, Galina Zdorovennova, Roman Zdorovennov, Nikolai Palshin, Andrey Mitrokhov
Format: Article
Language:English
Published: MDPI AG 2022-12-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/15/1/28
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author Sergey Bogdanov
Igor Maksimov
Galina Zdorovennova
Roman Zdorovennov
Nikolai Palshin
Andrey Mitrokhov
author_facet Sergey Bogdanov
Igor Maksimov
Galina Zdorovennova
Roman Zdorovennov
Nikolai Palshin
Andrey Mitrokhov
author_sort Sergey Bogdanov
collection DOAJ
description The calculation of the turbulent stress matrix using acoustic Doppler current profiler (ADCP) data remains a challenging problem in the study of geophysical flows. One of the ways to overcome the problem is to use a system of two coupled ADCP with pairs of beams intersecting at a certain depth. When device configuration is symmetric in horizontal, this setting makes it possible to estimate the stresses only for a small range of depths, close to the depth of beam intersection point. To overcome this restriction, in this paper the modified setting is proposed, when both devices are symmetrically turned in the horizontal plane. The X axes of the devices are not collinear for such setting, and two pairs of beams intersect at two different depths, which depend on the distance between the emitters and devices’ rotation angle, and can be chosen in advance. At each of these depths, six beam velocity variances can be directly calculated, as well as the correlation of those velocity components, which correspond to the intersecting beams. As a result, an overdetermined system of equations is derived for unknown stresses, for both depths. The method was approbated during the processing of two series of field data obtained in lakes during open water and ice-covered periods. In most cases, calculations lead to physically consistent results; in particular, the stress matrix turns out to be positive definite. The method’s limitations and perspectives of its development are discussed.
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spelling doaj.art-3c8c8f1fbb2a4c9399940d8efde338ce2023-12-02T01:13:13ZengMDPI AGWater2073-44412022-12-011512810.3390/w15010028Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPsSergey Bogdanov0Igor Maksimov1Galina Zdorovennova2Roman Zdorovennov3Nikolai Palshin4Andrey Mitrokhov5Northern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaNorthern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaNorthern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaNorthern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaNorthern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaNorthern Water Problems Institute, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya, 11, 185030 Petrozavodsk, RussiaThe calculation of the turbulent stress matrix using acoustic Doppler current profiler (ADCP) data remains a challenging problem in the study of geophysical flows. One of the ways to overcome the problem is to use a system of two coupled ADCP with pairs of beams intersecting at a certain depth. When device configuration is symmetric in horizontal, this setting makes it possible to estimate the stresses only for a small range of depths, close to the depth of beam intersection point. To overcome this restriction, in this paper the modified setting is proposed, when both devices are symmetrically turned in the horizontal plane. The X axes of the devices are not collinear for such setting, and two pairs of beams intersect at two different depths, which depend on the distance between the emitters and devices’ rotation angle, and can be chosen in advance. At each of these depths, six beam velocity variances can be directly calculated, as well as the correlation of those velocity components, which correspond to the intersecting beams. As a result, an overdetermined system of equations is derived for unknown stresses, for both depths. The method was approbated during the processing of two series of field data obtained in lakes during open water and ice-covered periods. In most cases, calculations lead to physically consistent results; in particular, the stress matrix turns out to be positive definite. The method’s limitations and perspectives of its development are discussed.https://www.mdpi.com/2073-4441/15/1/28lakeADCPturbulent stresses matrixover determined system of equationsstresses variations on vertical
spellingShingle Sergey Bogdanov
Igor Maksimov
Galina Zdorovennova
Roman Zdorovennov
Nikolai Palshin
Andrey Mitrokhov
Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
Water
lake
ADCP
turbulent stresses matrix
over determined system of equations
stresses variations on vertical
title Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
title_full Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
title_fullStr Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
title_full_unstemmed Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
title_short Towards Turbulent Stresses Estimates by Special Geometric Adjustment of Two ADCPs
title_sort towards turbulent stresses estimates by special geometric adjustment of two adcps
topic lake
ADCP
turbulent stresses matrix
over determined system of equations
stresses variations on vertical
url https://www.mdpi.com/2073-4441/15/1/28
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AT romanzdorovennov towardsturbulentstressesestimatesbyspecialgeometricadjustmentoftwoadcps
AT nikolaipalshin towardsturbulentstressesestimatesbyspecialgeometricadjustmentoftwoadcps
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