Large-eddy simulation of the generation and propagation of internal solitary waves

Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation resu...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Zhu, Hai [verfasserIn] Wang, LingLing [verfasserIn] Tang, HongWu [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	ISW DCEM internal wave generation bottom boundary layer LES boundary jets

Übergeordnetes Werk:	Enthalten in: Science in China - Heidelberg : Springer, 2003, 57(2014), 6 vom: 06. März, Seite 1128-1136
Übergeordnetes Werk:	volume:57 ; year:2014 ; number:6 ; day:06 ; month:03 ; pages:1128-1136

Links:	Volltext

DOI / URN:	10.1007/s11433-013-5231-1

Katalog-ID:	SPR019355920

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520			\|a Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets.
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allfields	10.1007/s11433-013-5231-1 doi (DE-627)SPR019355920 (SPR)s11433-013-5231-1-e DE-627 ger DE-627 rakwb eng 530 520 ASE 33.00 bkl 39.00 bkl Zhu, Hai verfasserin aut Large-eddy simulation of the generation and propagation of internal solitary waves 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets. ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213 Wang, LingLing verfasserin aut Tang, HongWu verfasserin aut Enthalten in Science in China Heidelberg : Springer, 2003 57(2014), 6 vom: 06. März, Seite 1128-1136 (DE-627)385614799 (DE-600)2142901-7 1862-2844 nnns volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136 https://dx.doi.org/10.1007/s11433-013-5231-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-AST SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 33.00 ASE 39.00 ASE AR 57 2014 6 06 03 1128-1136
spelling	10.1007/s11433-013-5231-1 doi (DE-627)SPR019355920 (SPR)s11433-013-5231-1-e DE-627 ger DE-627 rakwb eng 530 520 ASE 33.00 bkl 39.00 bkl Zhu, Hai verfasserin aut Large-eddy simulation of the generation and propagation of internal solitary waves 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets. ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213 Wang, LingLing verfasserin aut Tang, HongWu verfasserin aut Enthalten in Science in China Heidelberg : Springer, 2003 57(2014), 6 vom: 06. März, Seite 1128-1136 (DE-627)385614799 (DE-600)2142901-7 1862-2844 nnns volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136 https://dx.doi.org/10.1007/s11433-013-5231-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-AST SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 33.00 ASE 39.00 ASE AR 57 2014 6 06 03 1128-1136
allfields_unstemmed	10.1007/s11433-013-5231-1 doi (DE-627)SPR019355920 (SPR)s11433-013-5231-1-e DE-627 ger DE-627 rakwb eng 530 520 ASE 33.00 bkl 39.00 bkl Zhu, Hai verfasserin aut Large-eddy simulation of the generation and propagation of internal solitary waves 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets. ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213 Wang, LingLing verfasserin aut Tang, HongWu verfasserin aut Enthalten in Science in China Heidelberg : Springer, 2003 57(2014), 6 vom: 06. März, Seite 1128-1136 (DE-627)385614799 (DE-600)2142901-7 1862-2844 nnns volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136 https://dx.doi.org/10.1007/s11433-013-5231-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-AST SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 33.00 ASE 39.00 ASE AR 57 2014 6 06 03 1128-1136
allfieldsGer	10.1007/s11433-013-5231-1 doi (DE-627)SPR019355920 (SPR)s11433-013-5231-1-e DE-627 ger DE-627 rakwb eng 530 520 ASE 33.00 bkl 39.00 bkl Zhu, Hai verfasserin aut Large-eddy simulation of the generation and propagation of internal solitary waves 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets. ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213 Wang, LingLing verfasserin aut Tang, HongWu verfasserin aut Enthalten in Science in China Heidelberg : Springer, 2003 57(2014), 6 vom: 06. März, Seite 1128-1136 (DE-627)385614799 (DE-600)2142901-7 1862-2844 nnns volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136 https://dx.doi.org/10.1007/s11433-013-5231-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-AST SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 33.00 ASE 39.00 ASE AR 57 2014 6 06 03 1128-1136
allfieldsSound	10.1007/s11433-013-5231-1 doi (DE-627)SPR019355920 (SPR)s11433-013-5231-1-e DE-627 ger DE-627 rakwb eng 530 520 ASE 33.00 bkl 39.00 bkl Zhu, Hai verfasserin aut Large-eddy simulation of the generation and propagation of internal solitary waves 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets. ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213 Wang, LingLing verfasserin aut Tang, HongWu verfasserin aut Enthalten in Science in China Heidelberg : Springer, 2003 57(2014), 6 vom: 06. März, Seite 1128-1136 (DE-627)385614799 (DE-600)2142901-7 1862-2844 nnns volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136 https://dx.doi.org/10.1007/s11433-013-5231-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-AST SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 33.00 ASE 39.00 ASE AR 57 2014 6 06 03 1128-1136
language	English
source	Enthalten in Science in China 57(2014), 6 vom: 06. März, Seite 1128-1136 volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136
sourceStr	Enthalten in Science in China 57(2014), 6 vom: 06. März, Seite 1128-1136 volume:57 year:2014 number:6 day:06 month:03 pages:1128-1136
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	ISW DCEM internal wave generation bottom boundary layer LES boundary jets
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container_title	Science in China
authorswithroles_txt_mv	Zhu, Hai @@aut@@ Wang, LingLing @@aut@@ Tang, HongWu @@aut@@
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author	Zhu, Hai
spellingShingle	Zhu, Hai ddc 530 bkl 33.00 bkl 39.00 misc ISW misc DCEM misc internal wave generation misc bottom boundary layer misc LES misc boundary jets Large-eddy simulation of the generation and propagation of internal solitary waves
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topic_title	530 520 ASE 33.00 bkl 39.00 bkl Large-eddy simulation of the generation and propagation of internal solitary waves ISW (dpeaa)DE-He213 DCEM (dpeaa)DE-He213 internal wave generation (dpeaa)DE-He213 bottom boundary layer (dpeaa)DE-He213 LES (dpeaa)DE-He213 boundary jets (dpeaa)DE-He213
topic	ddc 530 bkl 33.00 bkl 39.00 misc ISW misc DCEM misc internal wave generation misc bottom boundary layer misc LES misc boundary jets
topic_unstemmed	ddc 530 bkl 33.00 bkl 39.00 misc ISW misc DCEM misc internal wave generation misc bottom boundary layer misc LES misc boundary jets
topic_browse	ddc 530 bkl 33.00 bkl 39.00 misc ISW misc DCEM misc internal wave generation misc bottom boundary layer misc LES misc boundary jets
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title	Large-eddy simulation of the generation and propagation of internal solitary waves
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title_full	Large-eddy simulation of the generation and propagation of internal solitary waves
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title_sort	large-eddy simulation of the generation and propagation of internal solitary waves
title_auth	Large-eddy simulation of the generation and propagation of internal solitary waves
abstract	Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets.
abstractGer	Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets.
abstract_unstemmed	Abstract A modified large-eddy simulation model, the dynamic coherent eddy model (DCEM) is employed to simulate the generation and propagation of internal solitary waves (ISWs) of both depression and elevation type, with wave amplitudes ranging from small, medium to large scales. The simulation results agree well with the existing experimental data. The generation process of ISWs is successfully captured by the DCEM method. Shear instabilities and diapycnal mixing in the initial wave generation phase are observed. The dissipation rate is not equal at different locations of an ISW. ISW-induced velocity field is analyzed in the present study. The structure of the bottom boundary layer (BBL) of internal wave packets is found to be different from that of a single ISW. A reverse boundary jet instead of a separation bubble exists behind the leading internal wave while separation bubbles appear in other parts of the wave-induced velocity field. The boundary jet flow resulting from the adverse pressure gradients has distinctive dynamics compared with free shear jets.
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title_short	Large-eddy simulation of the generation and propagation of internal solitary waves
url	https://dx.doi.org/10.1007/s11433-013-5231-1
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author2	Wang, LingLing Tang, HongWu
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up_date	2024-07-04T01:13:46.390Z
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