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Mars atmospheric entry is the entry into the atmosphere of Mars. High velocity entry into Martian air creates a CO2-N2 plasma, as opposed to O2-N2 for Earth air.
Mars entry is effected by the radiative effects of hot CO2 gas and Martian dust suspended in the air.
Flight regimes for entry, descent, and landing systems include aerocapture, hypersonic, supersonic, and subsonic.