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Designing a Martian UAV

Here, we share our engineering and scientific findings and reflect on our design-related choices

What atmospheric conditions are expected for the LEMFEV on Mars?

The Martian atmosphere is composed mainly of carbon dioxide (96% of CO2). The average surface pressure of the Martian atmosphere is about 1% of Earth's sea level pressure. The surface temperatures on Mars vary from -140 °C to +20 °C. Furthermore, strong winds (up to 5 m/s during the daytime) and turbulence can degrade aircraft efficiency and stability. The density at the surface of Mars is as low as that at an altitude of approximately 32 km above the Earth's surface. Figure 1 shows the distribution of nominal atmospheric density with altitude for Mars as compared to the data for the Earth's standard atmosphere.

Density vs Altitude.png

Figure 1 - Mars Nominal Atmosphere [1] and Earth Standard Atmosphere [2]:  Density vs Altitude

Density on Mars is highly variable depending on seasonal and daily cycles. During the daytime, it can fluctuate between 0.014 and 0.020 kg/m3.

The speed of sound on Mars is also lower than that on Earth due to the low temperature and different composition of the atmosphere; therefore, compressibility effects are more easily triggered. Figure 2 shows the dependence of the speed of sound on the altitude for Mars and Earth.

Figure 2 - Mars Nominal Atmosphere [1] and Earth Standard Atmosphere [2]:

Speed of Sound vs Altitude

Due to these specific environmental conditions, as well as unknown terrain elevation, limited knowledge of wind speed, dust storms, and rugged terrain, a Mars flying vehicle should possess some features different from those of an Earth aircraft.

References:

  1. NASA Technical Reports Server (NTRS) 20010056680: Mars Global Reference Atmospheric Model 2001 Version (Mars-GRAM 2001): Users Guide.

  2. International Standard Atmosphere - Wikipedia

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