A study of gravity waves on planetary atmospheres

Gravity waves (GWs) are internal atmospheric waves that exist on all planetary atmospheres and play an important role in atmospheric coupling, composition, variability, and structure. GWs transport energy and momentum from the lower to the upper atmosphere. GWs can influence upper atmospheric winds,...

Full description

Saved in:
Bibliographic Details
Main Author: Srivastava, Sarthak
Other Authors: Lee Yee Hui
Format: Thesis-Doctor of Philosophy
Language:English
Published: Nanyang Technological University 2023
Subjects:
Online Access:https://hdl.handle.net/10356/170351
Tags: Add Tag
No Tags, Be the first to tag this record!
Institution: Nanyang Technological University
Language: English
id sg-ntu-dr.10356-170351
record_format dspace
spelling sg-ntu-dr.10356-1703512023-10-03T09:52:45Z A study of gravity waves on planetary atmospheres Srivastava, Sarthak Lee Yee Hui School of Electrical and Electronic Engineering Amal Chandran EYHLee@ntu.edu.sg Science::Physics Engineering::Electrical and electronic engineering Gravity waves (GWs) are internal atmospheric waves that exist on all planetary atmospheres and play an important role in atmospheric coupling, composition, variability, and structure. GWs transport energy and momentum from the lower to the upper atmosphere. GWs can influence upper atmospheric winds, composition, contribute to turbulence and can play vital roles in influencing the mean circulation and thermal structure of the atmosphere. Despite the key influencing role of GW activity on planetary atmospheres, there is lack of a general numerical model for comparative numerical experimentation. Several numerical models for GW simulation on specific planets exist in the literature. Moreover, most of these models are either, too simplistic and make drastically simplifying assumptions, or they are detailed and require significant computational resources. This study aims to obtain a general understanding of the influence of GW activity on terrestrial planetary atmospheres via creation of a numerical model that is computationally lightweight yet captures the essential nonlinear GW dynamics. Intra-atmospheric coupling due to GWs is demonstrated by studying the GPS total electron content perturbations induced by waves triggered by the 2004 Sumatra Earthquakes. A two-dimensional nonlinear numerical model is then developed to study atmospheric coupling due to Acoustic Gravity Waves (AGWs) on different planets. The model is validated and applied to real case studies of tsunamigenic GWs on Earth and CO2 ice cloud formation on Mars. The model is further applied to evaluate the detectability of GWs from a spacecraft instrument. Finally, a parametric study is conducted to understand the influence of wave frequency on GW propagation across Earth, Venus, and Mars. Doctor of Philosophy 2023-09-08T05:00:33Z 2023-09-08T05:00:33Z 2023 Thesis-Doctor of Philosophy Srivastava, S. (2023). A study of gravity waves on planetary atmospheres. Doctoral thesis, Nanyang Technological University, Singapore. https://hdl.handle.net/10356/170351 https://hdl.handle.net/10356/170351 10.32657/10356/170351 en This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License (CC BY-NC 4.0). application/pdf Nanyang Technological University
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Science::Physics
Engineering::Electrical and electronic engineering
spellingShingle Science::Physics
Engineering::Electrical and electronic engineering
Srivastava, Sarthak
A study of gravity waves on planetary atmospheres
description Gravity waves (GWs) are internal atmospheric waves that exist on all planetary atmospheres and play an important role in atmospheric coupling, composition, variability, and structure. GWs transport energy and momentum from the lower to the upper atmosphere. GWs can influence upper atmospheric winds, composition, contribute to turbulence and can play vital roles in influencing the mean circulation and thermal structure of the atmosphere. Despite the key influencing role of GW activity on planetary atmospheres, there is lack of a general numerical model for comparative numerical experimentation. Several numerical models for GW simulation on specific planets exist in the literature. Moreover, most of these models are either, too simplistic and make drastically simplifying assumptions, or they are detailed and require significant computational resources. This study aims to obtain a general understanding of the influence of GW activity on terrestrial planetary atmospheres via creation of a numerical model that is computationally lightweight yet captures the essential nonlinear GW dynamics. Intra-atmospheric coupling due to GWs is demonstrated by studying the GPS total electron content perturbations induced by waves triggered by the 2004 Sumatra Earthquakes. A two-dimensional nonlinear numerical model is then developed to study atmospheric coupling due to Acoustic Gravity Waves (AGWs) on different planets. The model is validated and applied to real case studies of tsunamigenic GWs on Earth and CO2 ice cloud formation on Mars. The model is further applied to evaluate the detectability of GWs from a spacecraft instrument. Finally, a parametric study is conducted to understand the influence of wave frequency on GW propagation across Earth, Venus, and Mars.
author2 Lee Yee Hui
author_facet Lee Yee Hui
Srivastava, Sarthak
format Thesis-Doctor of Philosophy
author Srivastava, Sarthak
author_sort Srivastava, Sarthak
title A study of gravity waves on planetary atmospheres
title_short A study of gravity waves on planetary atmospheres
title_full A study of gravity waves on planetary atmospheres
title_fullStr A study of gravity waves on planetary atmospheres
title_full_unstemmed A study of gravity waves on planetary atmospheres
title_sort study of gravity waves on planetary atmospheres
publisher Nanyang Technological University
publishDate 2023
url https://hdl.handle.net/10356/170351
_version_ 1779171080915648512