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...

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Bibliographic Details
Published in:Atmosphere
Main Authors: Guangming Chen, Xie Li, Maosheng He, Shushi Liu, Haijun Man, Hong Gao, Yongping Li
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2023
Subjects:
thermospheric density
longitudinal distribution
dawn
dusk
low solar activity
APOD
Meteorology. Climatology
QC851-999
Geomagnetic Pole
Online Access:https://doi.org/10.3390/atmos14010155
https://doaj.org/article/6f8eb85df7e1489dabec5f0fc3bc232b
Description
Summary: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 (Δ ρ rmax ) near the geomagnetic pole, especially in the winter hemisphere. The annual maximum of Δ ρ rmax 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.

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