Related Experiment Video
Updated: Sep 4, 2025

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
Published on: May 29, 2019
Seasonal Variation of Thermospheric Composition Observed by NASA GOLD
Liying Qian1, Quan Gan2, Wenbin Wang1
1High Altitude Observatory National Center for Atmospheric Research Boulder CO USA.
Thermospheric composition shows asymmetric seasonal changes between hemispheres. These variations, influenced by factors like auroral heating, differ significantly with longitude and latitude.
Area of Science:
- Space Physics
- Atmospheric Science
- Geophysics
Background:
- Thermospheric composition is crucial for understanding Earth's upper atmosphere.
- Seasonal variations in the thermosphere are complex and influenced by solar activity and geomagnetic storms.
Purpose of the Study:
- To investigate the seasonal variation characteristics of thermospheric composition.
- To analyze hemispheric asymmetries and longitudinal dependencies in thermospheric composition.
Main Methods:
- Utilized column number density ratio (∑O/N₂) data from NASA's GOLD mission.
- Incorporated data from the GUVI instrument on TIMED satellite and NRLMSISE-00 empirical model.
- Analyzed seasonal patterns, hemispheric asymmetries, and longitudinal variations.
Main Results:
- Observed hemispheric asymmetry in ∑O/N₂ seasonal variation.
- Southern hemisphere shows annual and semiannual patterns; Northern hemisphere shows dominant annual variation with wintertime highs.
- Longitudinal variability in solstice season durations and latitude-dependent solstice-to-solstice changes in ∑O/N₂.
Conclusions:
- Ion-neutral collisional heating, ion drag, and auroral Joule heating likely cause longitudinal dependencies.
- Latitude significantly impacts the rate of thermospheric composition change between seasons.
More Related Videos
10:28Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
11:19Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
Published on: October 21, 2016
Related Concept Videos
Atomic Spectroscopy: Effects of Temperature
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature...
Variation of Atmospheric Pressure
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
Global Climate Change
Noble Gases
The elements in group 18 are noble gases (helium, neon, argon, krypton, xenon, and radon). They earned the name “noble” because they were assumed to be nonreactive since they have filled valence shells. In 1962, Dr. Neil Bartlett at the University of British Columbia proved this assumption to be false.
Inductively Coupled Plasma Atomic Emission Spectroscopy: Principle
The ions and electrons produced interact with the fluctuating magnetic field created by a water-cooled...
Atomic Absorption Spectroscopy: Lab
Solutions containing organic solvents, such as low-molecular-mass alcohols, esters, or ketones, enhance absorbances by increasing...