Solitonic interactions for Rossby waves with the influence of Coriolis parameters

In the current study, the Rossby waves envelope near the equator is studied starting from a potential vorticity equation with the horizontal component of Coriolis parameter. Based on the equation, we first establish the amplitude evolution equation of the Rossby waves with complete Coriolis paramete...

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Main Authors: XiaoJun Yin, QuanSheng Liu, ShengYun Ma, ShuTing Bai
Format: Article
Language:English
Published: Elsevier 2021-09-01
Series:Results in Physics
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2211379721006902
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spelling doaj-e070287e7f5f4e438c528f69407dd7992021-08-28T04:43:52ZengElsevierResults in Physics2211-37972021-09-0128104593Solitonic interactions for Rossby waves with the influence of Coriolis parametersXiaoJun Yin0QuanSheng Liu1ShengYun Ma2ShuTing Bai3College of Science, Inner Mongolia Agriculture University Hohhot 010018, ChinaSchool of Mathematical Science, Inner Mongolia University, Hohhot 010021, China; Corresponding author at: School of Mathematical Sciences, Inner Mongolia University, Hohhot, China.College of Science, Inner Mongolia Agriculture University Hohhot 010018, ChinaCollege of Science, Inner Mongolia Agriculture University Hohhot 010018, ChinaIn the current study, the Rossby waves envelope near the equator is studied starting from a potential vorticity equation with the horizontal component of Coriolis parameter. Based on the equation, we first establish the amplitude evolution equation of the Rossby waves with complete Coriolis parameter and obtain rational function solutions by means of the subsidiary ordinary differential equation method with the help of chirp-free hypothesis. Then the 1-, 2-, 3-and N-soliton solutions are also obtained by the Hirota method. For these obtained solutions, they are rarely mentioned in fluid mechanics of ocean and atmospheric motion. On the other hand, these three-dimensional stereograms of the 1-, 2-soliton solutions are depicted with the physical parameter changing. The influence of each parameter on wave amplitude, the peak position and propagation direction of Rossby waves are discussed. The results show that the horizontal Coriolis parameter only alter the phase shift of the Rossby waves amplitude for the 1-soliton and 2-soliton solution. These results are of great significance for further theoretical research in geophysical fluid.http://www.sciencedirect.com/science/article/pii/S2211379721006902Rossby wavesSolitonThe Hirota methodSubsidiary ordinary differential equation
collection DOAJ
language English
format Article
sources DOAJ
author XiaoJun Yin
QuanSheng Liu
ShengYun Ma
ShuTing Bai
spellingShingle XiaoJun Yin
QuanSheng Liu
ShengYun Ma
ShuTing Bai
Solitonic interactions for Rossby waves with the influence of Coriolis parameters
Results in Physics
Rossby waves
Soliton
The Hirota method
Subsidiary ordinary differential equation
author_facet XiaoJun Yin
QuanSheng Liu
ShengYun Ma
ShuTing Bai
author_sort XiaoJun Yin
title Solitonic interactions for Rossby waves with the influence of Coriolis parameters
title_short Solitonic interactions for Rossby waves with the influence of Coriolis parameters
title_full Solitonic interactions for Rossby waves with the influence of Coriolis parameters
title_fullStr Solitonic interactions for Rossby waves with the influence of Coriolis parameters
title_full_unstemmed Solitonic interactions for Rossby waves with the influence of Coriolis parameters
title_sort solitonic interactions for rossby waves with the influence of coriolis parameters
publisher Elsevier
series Results in Physics
issn 2211-3797
publishDate 2021-09-01
description In the current study, the Rossby waves envelope near the equator is studied starting from a potential vorticity equation with the horizontal component of Coriolis parameter. Based on the equation, we first establish the amplitude evolution equation of the Rossby waves with complete Coriolis parameter and obtain rational function solutions by means of the subsidiary ordinary differential equation method with the help of chirp-free hypothesis. Then the 1-, 2-, 3-and N-soliton solutions are also obtained by the Hirota method. For these obtained solutions, they are rarely mentioned in fluid mechanics of ocean and atmospheric motion. On the other hand, these three-dimensional stereograms of the 1-, 2-soliton solutions are depicted with the physical parameter changing. The influence of each parameter on wave amplitude, the peak position and propagation direction of Rossby waves are discussed. The results show that the horizontal Coriolis parameter only alter the phase shift of the Rossby waves amplitude for the 1-soliton and 2-soliton solution. These results are of great significance for further theoretical research in geophysical fluid.
topic Rossby waves
Soliton
The Hirota method
Subsidiary ordinary differential equation
url http://www.sciencedirect.com/science/article/pii/S2211379721006902
work_keys_str_mv AT xiaojunyin solitonicinteractionsforrossbywaveswiththeinfluenceofcoriolisparameters
AT quanshengliu solitonicinteractionsforrossbywaveswiththeinfluenceofcoriolisparameters
AT shengyunma solitonicinteractionsforrossbywaveswiththeinfluenceofcoriolisparameters
AT shutingbai solitonicinteractionsforrossbywaveswiththeinfluenceofcoriolisparameters
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