A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars
A two-dimensional nonlinear numerical model has been developed to study atmospheric coupling due to vertically propagating acoustic gravity waves (AGWs) on different planets. The model is able to simulate both acoustic and gravity waves due to inclusion of compressibility. The model also considers d...
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sg-ntu-dr.10356-1710012023-10-20T15:39:41Z A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars Srivastava, Sarthak Chandran, Amal Thiemann, Edward M. B. School of Electrical and Electronic Engineering Satellite Research Centre Engineering::Electrical and electronic engineering Acoustic Wave Wave Propagation A two-dimensional nonlinear numerical model has been developed to study atmospheric coupling due to vertically propagating acoustic gravity waves (AGWs) on different planets. The model is able to simulate both acoustic and gravity waves due to inclusion of compressibility. The model also considers dissipative effects due to viscosity, conduction, and radiative damping. The hyperbolic inviscid advection equations are solved using the Lax-Wendroff method. The parabolic diffusion terms are solved implicitly using a linear algebra-based Direct method. The model is validated by comparing numerical solutions against analytical results for linear propagation, critical level absorption, and mountain wave generation over an isolated hill. Acoustic wave generation in Martian atmosphere due to a pressure pulse is also demonstrated. A case study of tsunami-generated AGWs is presented for the 2004 Sumatra earthquake whereby the model is forced through tsunamigenic sea-surface displacement. The properties of simulated AGWs closely match those derived from ionospheric sounding observations reported in literature. Another application for Martian ice cloud formation is discussed where gravity waves from topographic sources are shown to create cold pockets with temperatures below the CO2 condensation threshold. The simulated cold pockets coincide with the cloud echo observations from the Mars Orbiting Laser Altimeter aboard Mars Global Survey spacecraft. Nanyang Technological University Published version The authors acknowledge funding support from NTU startup grant “a Cubesat for Earth Observations” 2023-10-14T07:04:51Z 2023-10-14T07:04:51Z 2022 Journal Article Srivastava, S., Chandran, A. & Thiemann, E. M. B. (2022). A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars. Journal of Geophysical Research: Planets, 127(8), e2021JE007156-. https://dx.doi.org/10.1029/2021JE007156 2169-9097 https://hdl.handle.net/10356/171001 10.1029/2021JE007156 2-s2.0-85136884643 8 127 e2021JE007156 en NTU-SUG Journal of Geophysical Research: Planets © 2022 American Geophysical Union. All rights reserved. This article may be downloaded for personal use only. Any other use requires prior permission of the copyright holder. The Version of Record is available online at http://doi.org/10.1029/2021JE007156 application/pdf |
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Engineering::Electrical and electronic engineering Acoustic Wave Wave Propagation Srivastava, Sarthak Chandran, Amal Thiemann, Edward M. B. A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
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A two-dimensional nonlinear numerical model has been developed to study atmospheric coupling due to vertically propagating acoustic gravity waves (AGWs) on different planets. The model is able to simulate both acoustic and gravity waves due to inclusion of compressibility. The model also considers dissipative effects due to viscosity, conduction, and radiative damping. The hyperbolic inviscid advection equations are solved using the Lax-Wendroff method. The parabolic diffusion terms are solved implicitly using a linear algebra-based Direct method. The model is validated by comparing numerical solutions against analytical results for linear propagation, critical level absorption, and mountain wave generation over an isolated hill. Acoustic wave generation in Martian atmosphere due to a pressure pulse is also demonstrated. A case study of tsunami-generated AGWs is presented for the 2004 Sumatra earthquake whereby the model is forced through tsunamigenic sea-surface displacement. The properties of simulated AGWs closely match those derived from ionospheric sounding observations reported in literature. Another application for Martian ice cloud formation is discussed where gravity waves from topographic sources are shown to create cold pockets with temperatures below the CO2 condensation threshold. The simulated cold pockets coincide with the cloud echo observations from the Mars Orbiting Laser Altimeter aboard Mars Global Survey spacecraft. |
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School of Electrical and Electronic Engineering |
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School of Electrical and Electronic Engineering Srivastava, Sarthak Chandran, Amal Thiemann, Edward M. B. |
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Article |
author |
Srivastava, Sarthak Chandran, Amal Thiemann, Edward M. B. |
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Srivastava, Sarthak |
title |
A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
title_short |
A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
title_full |
A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
title_fullStr |
A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
title_full_unstemmed |
A nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to Earth and Mars |
title_sort |
nonlinear numerical model for comparative study of acoustic-gravity wave propagation in planetary atmospheres: application to earth and mars |
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2023 |
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https://hdl.handle.net/10356/171001 |
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1781793728860520448 |