Mars Upper Level Winds Observed by MAVEN - Visualizations
- Visualizations by:
- Greg Shirah
- Scientific consulting by:
- Mehdi Benna
- View full credits
MAVEN is the first spacecraft specifically designed to study the Mars upper atmosphere, in order to better understand the evolution of its climate. These visualizations show MAVEN measuring the Martian upper level wind direction and magnitude over a series of thirty-three campaigns. In order for MAVEN to make these in-situ measurements, the spacecraft must be close to the upper atmosphere. The closest point of MAVEN's orbit to Mars (periapsis) dips into the tenuous upper reaches of the Martian thermosphere. The orbit also precesses over time to acquire measurements from different regions on the planet.
Now, scientists have used MAVEN data to map high-altitude wind currents on Mars for the first time. The data show that the Martian upper atmosphere is relatively independent of the daily rotation of Mars. On a day-to-day basis, high-altitude wind currents have a relatively fixed location with respect to the Sun, while Mars rotates underneath. Over the course of the Martian year, however, the currents follow the Sun north to south with the seasons.
MAVEN has also found that higher-elevation regions, such as the Tharsis plateau, cause small gravity waves that perturb the upper level winds and make them alter course. This means that certain topographic features on the Martian surface are detectable by MAVEN high above, as it skims the edge of space.
Now, scientists have used MAVEN data to map high-altitude wind currents on Mars for the first time. The data show that the Martian upper atmosphere is relatively independent of the daily rotation of Mars. On a day-to-day basis, high-altitude wind currents have a relatively fixed location with respect to the Sun, while Mars rotates underneath. Over the course of the Martian year, however, the currents follow the Sun north to south with the seasons.
MAVEN has also found that higher-elevation regions, such as the Tharsis plateau, cause small gravity waves that perturb the upper level winds and make them alter course. This means that certain topographic features on the Martian surface are detectable by MAVEN high above, as it skims the edge of space.
For More Information
See NASA.gov
Credits
Please give credit for this item to:
NASA/Goddard/SVS/MAVEN/CU Boulder/University of Michigan
Visualizers
- Greg Shirah (NASA/GSFC) [Lead]
- Ernie Wright (USRA)
- Horace Mitchell (NASA/GSFC)
Scientists
- Mehdi Benna (UMBC) [Lead]
- Kali Roeten (University of Michigan)
Producer
- Dan Gallagher (KBRwyle)
Technical support
- Ian Jones (ADNET)
- Laurence Schuler (ADNET)
Missions
This visualization is related to the following missions:Datasets used in this visualization
MGS (Collected with the MOC sensor)
MAVEN NGIMS (A.K.A. Average Neutral Upper Level Wind Vectors) (Collected with the Neutral Gas and Ion Mass Spectrometer sensor)
Observed DataNASA
Average neutral winds as observed by MAVEN/NGIMS during 33 monthly campaigns spanning from April 2016 to December 2018.
Credit: NGIMS: MAVEN Science Team
See more visualizations using this data setCelesTrak Spacecraft Orbit Ephemeris
Ephemeris
Dataset can be found at: http://celestrak.com
See more visualizations using this data setHipparcos Tycho Catalogue (A.K.A. Tycho 2 Catalogue) (Collected with the Telescope sensor)
Database
Dataset can be found at: http://archive.eso.org/ASTROM/
See more visualizations using this data setNote: While we identify the data sets used in these visualizations, we do not store any further details nor the data sets themselves on our site.
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