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Updated: Mar 30, 2026

Scattering And Absorption of Light in Planetary Regoliths
Published on: July 1, 2019
Dust observations at orbital altitudes surrounding Mars.
L Andersson1, T D Weber2, D Malaspina2
1Laboratory for Atmospheric and Space Physics, University of Colorado-Boulder, Boulder, CO 80303, USA. laila.andersson@lasp.colorado.edu.
Interplanetary dust particles have been observed entering Mars's atmosphere at high altitudes. This discovery challenges previous assumptions about dust transport and impacts our understanding of the inner solar system.
Area of Science:
- Planetary Science
- Atmospheric Science
- Astrogeology
Background:
- Dust is prevalent near Mars's surface, but its presence at high altitudes (>150 km) was unexplained by known atmospheric processes.
- Previous models did not account for significant dust concentrations at altitudes above 150 kilometers on Mars.
Purpose of the Study:
- To investigate the presence and origin of dust at high altitudes in the Martian atmosphere.
- To analyze the characteristics of observed dust particles and their implications for interplanetary dust dynamics.
Main Methods:
- Utilized the Langmuir Probe and Wave instrument aboard the Mars Atmosphere and Volatile Evolution (MAVEN) spacecraft.
- Analyzed dust distribution data from 150 km to over 1000 km altitude.
- Compared observational data with laboratory measurements of dust properties.
Main Results:
- Detected dust at altitudes significantly higher than previously thought possible, ranging from 150 to over 1000 km.
- Interpreted the observed dust distribution as indicative of interplanetary origin.
- Estimated dust grain sizes between 1 and 12 micrometers, assuming a velocity of ~18 km/s.
Conclusions:
- Confirmed the presence of interplanetary dust entering the Martian atmosphere at high altitudes.
- Provided direct evidence improving understanding of interplanetary dust sources, sinks, and transport in the inner solar system.
- Highlighted the impact of this dust on Mars's atmospheric processes.
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