2D and 3D Properties of Stably Stratified Turbulence

Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably st...
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Gespeichert in:

Autor*in:	Yoshifumi Kimura [verfasserIn] Peter P. Sullivan [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2024

Schlagwörter:	stratified turbulence buoyancy scale Ozmidov scale Kolmogorov scale Craya-Herring decomposition temperature front

Übergeordnetes Werk:	In: Atmosphere - MDPI AG, 2011, 15(2024), 1, p 82
Übergeordnetes Werk:	volume:15 ; year:2024 ; number:1, p 82

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/atmos15010082

Katalog-ID:	DOAJ096393491

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spelling	10.3390/atmos15010082 doi (DE-627)DOAJ096393491 (DE-599)DOAJ81b95eca74294d128e6664599f1da5e9 DE-627 ger DE-627 rakwb eng QC851-999 Yoshifumi Kimura verfasserin aut 2D and 3D Properties of Stably Stratified Turbulence 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably stratified turbulence. After reviewing the importance of three characteristic length scales and their relations in stably stratified turbulence, we present numerical results showing how structures and spectra develop with the growth of the length scales. It is demonstrated that the temperature fluctuations make sharp fronts vertically which result in non-symmetric PDFs of the vertical derivative <inline-formula<<math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"<<semantics<<mrow<<msub<<mo<∂</mo<<mi<z</mi<</msub<<mi<θ</mi<</mrow<</semantics<</math<</inline-formula<. stratified turbulence buoyancy scale Ozmidov scale Kolmogorov scale Craya-Herring decomposition temperature front Meteorology. Climatology Peter P. Sullivan verfasserin aut In Atmosphere MDPI AG, 2011 15(2024), 1, p 82 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:15 year:2024 number:1, p 82 https://doi.org/10.3390/atmos15010082 kostenfrei https://doaj.org/article/81b95eca74294d128e6664599f1da5e9 kostenfrei https://www.mdpi.com/2073-4433/15/1/82 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 1, p 82
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allfieldsSound	10.3390/atmos15010082 doi (DE-627)DOAJ096393491 (DE-599)DOAJ81b95eca74294d128e6664599f1da5e9 DE-627 ger DE-627 rakwb eng QC851-999 Yoshifumi Kimura verfasserin aut 2D and 3D Properties of Stably Stratified Turbulence 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably stratified turbulence. After reviewing the importance of three characteristic length scales and their relations in stably stratified turbulence, we present numerical results showing how structures and spectra develop with the growth of the length scales. It is demonstrated that the temperature fluctuations make sharp fronts vertically which result in non-symmetric PDFs of the vertical derivative <inline-formula<<math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"<<semantics<<mrow<<msub<<mo<∂</mo<<mi<z</mi<</msub<<mi<θ</mi<</mrow<</semantics<</math<</inline-formula<. stratified turbulence buoyancy scale Ozmidov scale Kolmogorov scale Craya-Herring decomposition temperature front Meteorology. Climatology Peter P. Sullivan verfasserin aut In Atmosphere MDPI AG, 2011 15(2024), 1, p 82 (DE-627)657584010 (DE-600)2605928-9 20734433 nnns volume:15 year:2024 number:1, p 82 https://doi.org/10.3390/atmos15010082 kostenfrei https://doaj.org/article/81b95eca74294d128e6664599f1da5e9 kostenfrei https://www.mdpi.com/2073-4433/15/1/82 kostenfrei https://doaj.org/toc/2073-4433 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2014 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 15 2024 1, p 82
language	English
source	In Atmosphere 15(2024), 1, p 82 volume:15 year:2024 number:1, p 82
sourceStr	In Atmosphere 15(2024), 1, p 82 volume:15 year:2024 number:1, p 82
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	stratified turbulence buoyancy scale Ozmidov scale Kolmogorov scale Craya-Herring decomposition temperature front Meteorology. Climatology
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container_title	Atmosphere
authorswithroles_txt_mv	Yoshifumi Kimura @@aut@@ Peter P. Sullivan @@aut@@
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callnumber-first	Q - Science
author	Yoshifumi Kimura
spellingShingle	Yoshifumi Kimura misc QC851-999 misc stratified turbulence misc buoyancy scale misc Ozmidov scale misc Kolmogorov scale misc Craya-Herring decomposition misc temperature front misc Meteorology. Climatology 2D and 3D Properties of Stably Stratified Turbulence
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topic_title	QC851-999 2D and 3D Properties of Stably Stratified Turbulence stratified turbulence buoyancy scale Ozmidov scale Kolmogorov scale Craya-Herring decomposition temperature front
topic	misc QC851-999 misc stratified turbulence misc buoyancy scale misc Ozmidov scale misc Kolmogorov scale misc Craya-Herring decomposition misc temperature front misc Meteorology. Climatology
topic_unstemmed	misc QC851-999 misc stratified turbulence misc buoyancy scale misc Ozmidov scale misc Kolmogorov scale misc Craya-Herring decomposition misc temperature front misc Meteorology. Climatology
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title	2D and 3D Properties of Stably Stratified Turbulence
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title_full	2D and 3D Properties of Stably Stratified Turbulence
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title_sort	2d and 3d properties of stably stratified turbulence
callnumber	QC851-999
title_auth	2D and 3D Properties of Stably Stratified Turbulence
abstract	Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably stratified turbulence. After reviewing the importance of three characteristic length scales and their relations in stably stratified turbulence, we present numerical results showing how structures and spectra develop with the growth of the length scales. It is demonstrated that the temperature fluctuations make sharp fronts vertically which result in non-symmetric PDFs of the vertical derivative <inline-formula<<math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"<<semantics<<mrow<<msub<<mo<∂</mo<<mi<z</mi<</msub<<mi<θ</mi<</mrow<</semantics<</math<</inline-formula<.
abstractGer	Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably stratified turbulence. After reviewing the importance of three characteristic length scales and their relations in stably stratified turbulence, we present numerical results showing how structures and spectra develop with the growth of the length scales. It is demonstrated that the temperature fluctuations make sharp fronts vertically which result in non-symmetric PDFs of the vertical derivative <inline-formula<<math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"<<semantics<<mrow<<msub<<mo<∂</mo<<mi<z</mi<</msub<<mi<θ</mi<</mrow<</semantics<</math<</inline-formula<.
abstract_unstemmed	Through interactions between the modes of “waves” and “vortices”, stably stratified turbulence exhibits characteristic features both in 2D and 3D. Using DNS of the Navier–Stokes equations coupled to an equation for temperature (the Bousinessq system), we investigate dynamical properties of stably stratified turbulence. After reviewing the importance of three characteristic length scales and their relations in stably stratified turbulence, we present numerical results showing how structures and spectra develop with the growth of the length scales. It is demonstrated that the temperature fluctuations make sharp fronts vertically which result in non-symmetric PDFs of the vertical derivative <inline-formula<<math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"<<semantics<<mrow<<msub<<mo<∂</mo<<mi<z</mi<</msub<<mi<θ</mi<</mrow<</semantics<</math<</inline-formula<.
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title_short	2D and 3D Properties of Stably Stratified Turbulence
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