Impacts of SABER CO2-based eddy diffusion coefficients in the lower thermosphere on the ionosphere/thermosphere

NCUIR > College of Earth Sciences > DEPARTMENT OF SPACE SCIENCE AND ENGINEERING > journal & Dissertation > Item 987654321/102211

Please use this identifier to cite or link to this item: https://ir.lib.ncu.edu.tw/handle/987654321/102211

Title:	Impacts of SABER CO2-based eddy diffusion coefficients in the lower thermosphere on the ionosphere/thermosphere
Authors:	張起維;Salinas, Cornelius Csar Jude H.;Chang, Loren C.;Liang, Mao‐Chang;Yue, Jia;Russell, James;Mlynczak, Martin
Contributors:	地球科學學院太空科學與工程學系
Keywords:	Atmospheric forcing;Boundary conditions;Broadband;Carbon dioxide;Diffusion;Diffusion coefficient;Eddy diffusion;Electrodynamics;General circulation models;Gravitational waves;Gravity waves;Ionosphere;ionospheric electron density;Ionospheric models;Lower thermosphere;Mesosphere;MLT region;Oscillations;Parameterization;Radiometry;Seasonal variations;Semiannual oscillation;Thermosphere;thermospheric density;Vortices;Wave breaking
Date:	2016-12-01
Issue Date:	2026-04-23 11:04:14 (UTC+8)
Publisher:	Wiley-Blackwell;Washington: Blackwell Publishing Ltd
Abstract:	摘要： This work estimates global‐mean Kzz using Sounding of the Atmosphere using Broadband Emission Radiometry/Thermosphere‐Ionosphere‐Mesosphere Energetics and Dynamics monthly global‐mean CO2 profiles and a one‐dimensional transport model. It is then specified as a lower boundary into the Thermosphere‐Ionosphere‐Electrodynamics General Circulation Model (TIE‐GCM). Results first show that global‐mean CO2 in the mesosphere and lower thermosphere region has annual and semiannual oscillations (AO and SAO) with maxima during solstice seasons along with a primary maximum in boreal summer. Our calculated AO and SAO in global‐mean CO2 are then modeled by AO and SAO in global‐mean Kzz. It is then shown that our estimated global‐mean Kzz is lower in magnitude than the suggested global‐mean Kzz from Qian et al. (2009) that can model the observed AO and SAO in the ionosphere/thermosphere (IT) region. However, our estimated global‐mean Kzz is similar in magnitude with recent suggestions of global‐mean Kzz in models with explicit gravity wave parameterization. Our work therefore concludes that global‐mean Kzz from global‐mean CO2 profiles cannot model the observed AO and SAO in the IT region because our estimated global‐mean Kzz may only be representing eddy diffusion due to gravity wave breaking. The difference between our estimated global‐mean Kzz and the global‐mean Kzz from Qian et al. (2009) thus represents diffusion and mixing from other nongravity wave sources not directly accounted for in the TIE‐GCM lower boundary conditions. These other sources may well be the more dominant lower atmospheric forcing behind the AO and SAO in the IT region. Key Points Global‐mean CO2 has annual and semiannual oscillations Seasonal variation of global‐mean Kzz estimated from global‐mean CO2 Global‐mean Kzz from CO2 alone cannot reproduce annual and semiannual oscillations in IT region 出版者： Washington: Blackwell Publishing Ltd 出版日期： 2016-12 出處： Journal of geophysical research : Space physics (2013 - Present), 2016-12, Vol.121 (12), p.12,080-12,092 資源來源： Wiley Online Library 版權： 2016. American Geophysical Union. All Rights Reserved. 識別號： ISSN: 2169-9380 識別號： EISSN: 2169-9402 識別號： DOI: 10.1002/2016JA023161
Appears in Collections:	[DEPARTMENT OF SPACE SCIENCE AND ENGINEERING] journal & Dissertation

Files in This Item:

File	Description	Size	Format
index.html		0Kb	HTML	36	View/Open

社群 sharing

Loading...