Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity
The symmetry reduction equations, similarity solutions, sub-groups and exact solutions of the (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity (INHBV equations), which describe the atmospheric gravity waves, are researched in this paper. Calculation on s...
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Online Access: | http://dx.doi.org/10.1063/1.4929574 |
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doaj-dd9e601da0724542a29f693ce729022e2020-11-25T01:27:42ZengAIP Publishing LLCAIP Advances2158-32262015-08-0158087162087162-1510.1063/1.4929574061508ADVExact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosityPing Liu0Bao-Qing Zeng1Bo-Bo Deng2Jian-Rong Yang3School of Physical Electronics, University of Electronic Science and Technology of China, Chengdu 610054, ChinaSchool of Physical Electronics, University of Electronic Science and Technology of China, Chengdu 610054, ChinaSchool of Physical Electronics, University of Electronic Science and Technology of China, Chengdu 610054, ChinaDepartment of Physics and Electronics, Shangrao Normal University, Shangrao 334001, ChinaThe symmetry reduction equations, similarity solutions, sub-groups and exact solutions of the (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity (INHBV equations), which describe the atmospheric gravity waves, are researched in this paper. Calculation on symmetry shows that the equations are invariant under the Galilean transformations, scaling transformations, rotational transformations and space-time translations. Three types of symmetry reduction equations and similar solutions for the (3+1)-dimensional INHBV equations are proposed. Traveling wave solutions of the INHBV equations are demonstrated by means of symmetry method. The evolutions on the wind velocities and temperature perturbation are demonstrated by figures.http://dx.doi.org/10.1063/1.4929574 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ping Liu Bao-Qing Zeng Bo-Bo Deng Jian-Rong Yang |
spellingShingle |
Ping Liu Bao-Qing Zeng Bo-Bo Deng Jian-Rong Yang Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity AIP Advances |
author_facet |
Ping Liu Bao-Qing Zeng Bo-Bo Deng Jian-Rong Yang |
author_sort |
Ping Liu |
title |
Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity |
title_short |
Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity |
title_full |
Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity |
title_fullStr |
Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity |
title_full_unstemmed |
Exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity |
title_sort |
exact solutions of atmospheric (3+1)-dimensional nonlinear incompressible non-hydrostatic boussinesq equations with viscosity |
publisher |
AIP Publishing LLC |
series |
AIP Advances |
issn |
2158-3226 |
publishDate |
2015-08-01 |
description |
The symmetry reduction equations, similarity solutions, sub-groups and exact solutions of the (3+1)-dimensional nonlinear incompressible non-hydrostatic Boussinesq equations with viscosity (INHBV equations), which describe the atmospheric gravity waves, are researched in this paper. Calculation on symmetry shows that the equations are invariant under the Galilean transformations, scaling transformations, rotational transformations and space-time translations. Three types of symmetry reduction equations and similar solutions for the (3+1)-dimensional INHBV equations are proposed. Traveling wave solutions of the INHBV equations are demonstrated by means of symmetry method. The evolutions on the wind velocities and temperature perturbation are demonstrated by figures. |
url |
http://dx.doi.org/10.1063/1.4929574 |
work_keys_str_mv |
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1725103740481961984 |