Every Mars landing is a knuckle-whitening feat of engineering. But each attempt has its own quirks based on where a spacecraft is going and what kind of science the mission intends to gather.
On Nov. 26, NASA will try to safely set a new spacecraft on Mars. InSight is a lander dedicated to studying the deep interior of the planet – the first mission ever to do so.
Here are a few things to know about InSight’s landing.
Landing on Mars is hard
Only about 40 percent of the missions ever sent to Mars – by any space agency – have been successful. The U.S. is the only nation whose missions have survived a Mars landing. The thin atmosphere – just 1 percent of Earth’s – means that there’s little friction to slow down a spacecraft. Despite that, NASA has had a long and successful track record at Mars. Since 1965, it has flown by, orbited, landed on and roved across the surface of the Red Planet.
InSight uses tried-and-true technology
In 2008, NASA’s Jet Propulsion Laboratory in Pasadena, California, successfully landed the Phoenix spacecraft at Mars’ North Pole. InSight is based on the Phoenix spacecraft, both of which were built by Lockheed Martin Space in Denver. Despite tweaks to its heat shield and parachute, the overall landing design is still very much the same: After separating from a cruise stage, an aeroshell descends through the atmosphere. The parachute and retrorockets slow the spacecraft down, and suspended legs absorb some shock from the touchdown.
InSight is landing on “the biggest parking lot on Mars”
One of the benefits of InSight’s science instruments is that they can record equally valuable data regardless of where they are on the planet. That frees the mission from needing anything more complicated than a flat, solid surface (ideally with few boulders and rocks). For the mission’s team, the landing site at Elysium Planitia is sometimes thought as “the biggest parking lot on Mars.”
InSight was built to land in a dust storm
InSight’s engineers have built a tough spacecraft, able to touch down safely in a dust storm if it needs to. The spacecraft’s heat shield is designed to be thick enough to withstand being “sandblasted” by dust. Its parachute has suspension lines that were tested to be stronger than Phoenix’s, in case it faces more air resistance due to the atmospheric conditions expected during a dust storm.
The entry, descent and landing sequence also has some flexibility to handle shifting weather. The mission team will be receiving daily weather updates from NASA’s Mars Reconnaissance Orbiter in the days before landing so that they can tweak when InSight’s parachute deploys and when it uses radar to find the Martian surface.
After landing, InSight will provide new science about rocky planets
InSight will teach us about the interior of planets like our own. The mission team hopes that by studying the deep interior of Mars, we can learn how other rocky worlds, including Earth and the Moon, formed. Our home planet and Mars were molded from the same primordial stuff more than 4.5 billion years ago but then became quite different. Why didn’t they share the same fate?
When it comes to rocky planets, we’ve only studied one in detail: Earth. By comparing Earth’s interior to that of Mars, InSight’s team members hope to better understand our solar system. What they learn might even aid the search for Earth-like exoplanets, narrowing down which ones might be able to support life. So while InSight is a Mars mission, it’s also much more than a Mars mission.
JPL manages InSight for NASA’s Science Mission Directorate. InSight is part of NASA’s Discovery Program, managed by the agency’s Marshall Space Flight Center in Huntsville, Alabama. Lockheed Martin Space in Denver built the InSight spacecraft, including its cruise stage and lander, and supports spacecraft operations for the mission.
A number of European partners, including France’s Centre National d’Études Spatiales (CNES) and the German Aerospace Center (DLR), are supporting the InSight mission. CNES provided the Seismic Experiment for Interior Structure (SEIS) instrument, with significant contributions from the Max Planck Institute for Solar System Research (MPS) in Germany, the Swiss Institute of Technology (ETH) in Switzerland, Imperial College and Oxford University in the United Kingdom, and JPL. DLR provided the Heat Flow and Physical Properties Package (HP3) instrument, with significant contributions from the Polish Space Agency (CBK) and Astronika in Poland. Spain’s Centro de Astrobiología (CAB) supplied the wind sensors.
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