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James Webb goes deep into the temperature and atmosphere of Mars digital trends

James Webb goes deep into the temperature and atmosphere of Mars  digital trends
Written by adrina

Although the James Webb Space Telescope was built primarily for looking back at the earliest and most distant galaxies, it can also be used for a variety of other scientific observations – including looking at targets right here in our own solar system. Webb will be conducting a major study of Jupiter and has already photographed Neptune. Now Webb has been used to take a fascinating look at our planetary neighbor Mars.

It’s actually quite difficult for Webb to study Mars because it’s so close and therefore very bright in both the visible light part of the spectrum and the infrared wavelengths where Webb observes. The brightness can oversaturate the detectors, which are designed to pick up very faint light sources. But Webb’s NIRCam camera was able to image the Martian surface, with two images at different wavelengths shown below.

Webb’s first images of Mars, taken by his NIRCam instrument on September 5, 2022 [Guaranteed Time Observation Program 1415]. Left: Reference map of the observed Martian hemisphere from NASA and the Mars Orbiter Laser Altimeter (MOLA). Top right: NIRCam image showing 2.1 micron (F212 filter) reflected sunlight revealing surface features such as craters and dust layers. Bottom right: Simultaneous NIRCam image showing ~4.3 microns (F430M filter) emitted light showing temperature differences with latitude and time of day, and darkening of the Hellas Basin caused by atmospheric effects. The light yellow area is just at the saturation limit of the detector. NASA, ESA, CSA, STScI, Mars JWST/GTO team

The shorter-wavelength image shown above is similar to a visible-light image, showing features such as craters and basins. The longer-wavelength image shown below shows how the planet radiates heat. The brightest point is where the sun is directly overhead, with cooler regions toward the poles. The Hellas Basin also appears darker, but this is not due to temperature effects, but rather to altitude and air pressure effects.

Webb was also able to capture Mars with his spectrometry instruments. These can split light into different wavelengths to see the composition of an object – in this case, the composition of the Martian atmosphere as a whole. There’s strong evidence for carbon dioxide, water, and carbon monoxide, and what’s impressive about it is how well the data fits the model we already know of the Martian atmosphere. This shows how effective Webb’s instruments are for this type of spectrometry work – and how effective Webb’s potential is when it comes to studying the atmospheres of exoplanets.

Webb's first near-infrared spectrum of Mars taken with the near-infrared spectrograph.
Webb’s first near-infrared spectrum of Mars acquired by the near-infrared spectrograph (NIRSpec) on September 5, 2022 as part of Guaranteed Time Observation Program 1415 over 3 slotted gratings (G140H, G235H, G395H). The spectrum is dominated by reflected sunlight at wavelengths shorter than 3 microns and thermal emission at longer wavelengths. Preliminary analysis shows that the spectral dips occur at specific wavelengths where light is absorbed by molecules in the Martian atmosphere, specifically carbon dioxide, carbon monoxide, and water. Other details provide information about dust, clouds and surface features. By constructing a best-fit model of the spectrum, such as the Planetary Spectrum Generator, the abundance of certain molecules in the atmosphere can be derived. NASA, ESA, CSA, STScI, Mars JWST/GTO team

Research using this Webb data is ongoing and has not yet been published or peer-reviewed, so it should not be considered definitive. But it shows how versatile a tool Webb can be as more Webb data on Mars is to come.

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