Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations

The longitudinal distribution of upper atmospheric density has been broadly studied. However, the studies mostly focused on 24 h averaged distribution. This study presents the longitudinal distribution of thermospheric density at dawn and dusk, using observations collected by the atmospheric density...

Full description

Bibliographic Details
Published in:Atmosphere
Main Authors: Guangming Chen, Xie Li, Maosheng He, Shushi Liu, Haijun Man, Hong Gao, Yongping Li
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/atmos14010155
id ftmdpi:oai:mdpi.com:/2073-4433/14/1/155/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2073-4433/14/1/155/ 2023-08-20T04:06:38+02:00 Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations Guangming Chen Xie Li Maosheng He Shushi Liu Haijun Man Hong Gao Yongping Li agris 2023-01-10 application/pdf https://doi.org/10.3390/atmos14010155 EN eng Multidisciplinary Digital Publishing Institute Upper Atmosphere https://dx.doi.org/10.3390/atmos14010155 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 1; Pages: 155 thermospheric density longitudinal distribution dawn dusk low solar activity APOD Text 2023 ftmdpi https://doi.org/10.3390/atmos14010155 2023-08-01T08:13:30Z The longitudinal distribution of upper atmospheric density has been broadly studied. However, the studies mostly focused on 24 h averaged distribution. This study presents the longitudinal distribution of thermospheric density at dawn and dusk, using observations collected by the atmospheric density detector onboard the Chinese satellite APOD (Atmospheric Density Detection and Precise Orbit Determination) during low solar activity. The APOD observations show a significant relative longitudinal variation of thermospheric density with global maxima (Δρrmax) near the geomagnetic pole, especially in the winter hemisphere. The annual maximum of Δρrmax appears in the Southern Hemisphere around the June solstices and reaches 26.3% and 39.6% at dawn and dusk, respectively. The auroral heating and meridional wind might play a significant role in the longitudinal variation of thermospheric density. We further compare the APOD observations with the semi-empirical atmospheric model MSIS (Mass Spectrometer Incoherent Scatter Radar) 2.0 predictions under low solar activity conditions. The MSIS 2.0 model reproduces similar longitudinal variations to the observations, with hemispheric asymmetry. The longitudinal variation of thermospheric density from APOD should be related to the distribution of the atmospheric average molecular weight from the model. More observational data are needed to verify the results of this study further. Text Geomagnetic Pole MDPI Open Access Publishing Atmosphere 14 1 155
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic thermospheric density
longitudinal distribution
dawn
dusk
low solar activity
APOD
spellingShingle thermospheric density
longitudinal distribution
dawn
dusk
low solar activity
APOD
Guangming Chen
Xie Li
Maosheng He
Shushi Liu
Haijun Man
Hong Gao
Yongping Li
Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
topic_facet thermospheric density
longitudinal distribution
dawn
dusk
low solar activity
APOD
description The longitudinal distribution of upper atmospheric density has been broadly studied. However, the studies mostly focused on 24 h averaged distribution. This study presents the longitudinal distribution of thermospheric density at dawn and dusk, using observations collected by the atmospheric density detector onboard the Chinese satellite APOD (Atmospheric Density Detection and Precise Orbit Determination) during low solar activity. The APOD observations show a significant relative longitudinal variation of thermospheric density with global maxima (Δρrmax) near the geomagnetic pole, especially in the winter hemisphere. The annual maximum of Δρrmax appears in the Southern Hemisphere around the June solstices and reaches 26.3% and 39.6% at dawn and dusk, respectively. The auroral heating and meridional wind might play a significant role in the longitudinal variation of thermospheric density. We further compare the APOD observations with the semi-empirical atmospheric model MSIS (Mass Spectrometer Incoherent Scatter Radar) 2.0 predictions under low solar activity conditions. The MSIS 2.0 model reproduces similar longitudinal variations to the observations, with hemispheric asymmetry. The longitudinal variation of thermospheric density from APOD should be related to the distribution of the atmospheric average molecular weight from the model. More observational data are needed to verify the results of this study further.
format Text
author Guangming Chen
Xie Li
Maosheng He
Shushi Liu
Haijun Man
Hong Gao
Yongping Li
author_facet Guangming Chen
Xie Li
Maosheng He
Shushi Liu
Haijun Man
Hong Gao
Yongping Li
author_sort Guangming Chen
title Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
title_short Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
title_full Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
title_fullStr Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
title_full_unstemmed Longitudinal Variation of Thermospheric Density during Low Solar Activity from APOD Observations
title_sort longitudinal variation of thermospheric density during low solar activity from apod observations
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/atmos14010155
op_coverage agris
genre Geomagnetic Pole
genre_facet Geomagnetic Pole
op_source Atmosphere; Volume 14; Issue 1; Pages: 155
op_relation Upper Atmosphere
https://dx.doi.org/10.3390/atmos14010155
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos14010155
container_title Atmosphere
container_volume 14
container_issue 1
container_start_page 155
_version_ 1774717874868322304