Mars Odyssey

http://marsprogram.jpl.nasa.gov/odyssey/

 

 

File written by Adobe Photoshop® 5.0

 

 

Launched on April 7, 2001, the 2001 Mars Odyssey spacecraft was designed with a greater emphasis on infrared mapping at higher spatial resolutions than that the MGS was. The Mars Odyssey instrumentation is briefly described here:

http://marsprogram.jpl.nasa.gov/odyssey/mission/instruments.html

 

 

 

 

Thermal Emission Imaging System (THEMIS). http://themis.asu.edu/

 

This imager combines 5 visible bands with 10 infrared bands. The wavelengths were chosen to be centered in various diagnostic bands for minerals. The spatial resolution is not as fine as the highest-resolution visible-light images of the MGS, but is superior to the IR mapper of MGS. Typical spatial resolutions are about 20 m at visual wavelengths and 100 m in the IR. The TES (http://tes.asu.edu/) on the MGS has a resolution of 3 km. However, the TES could also obtain spectra with a resolution of 5-10 cm-1.

 

 

 

A comparison of the spatial resolution of the thermal imagers on MGS (left) and MO (right).

 

 

 

 

 

 

 

 

 

 

 

 

 

“Etched terrain” in Meridiani Planum. Note that here light and dark do not indicate the light reflected and absorbed (or shadowed), respectively, but rather differences in temperature.

 

THEMIS IR images of Gusev Crater draped over MGS topography data. Temperatures run from 45 °C (black) to -5°C (white) and are due to differences in illumination. We will come back to Gusev twice more….

 

 

 

 

 

 

Left: Image of layered terrain in Candor Chasma, a canyon just north of Vallis Marineris and part of the general VM complex.

 

Right: Location of the image compared to a wider image of the Candor Chasma region, to “place it in context”.

 

 

 

 

 

The THEMIS image gallery is filled with these images and their “contexts”: http://marsprogram.jpl.nasa.gov/odyssey/gallery/latestimages/index.html

 

Neutron Spectrometer

 

MO also carried a neutron spectrometer. This detects the presence of hydrogen near the surface. Since water is generally the most abundant source of hydrogen, it maps (sort of) the distribution of water near the surface of the planet.

To see a full-blown version of this map, I dare you to go download the full image, or click on:

http://marsprogram.jpl.nasa.gov/odyssey/gallery/latestimages/latest2003/jul/20030724a-01.jpg

DO NOT TRY THIS WITH A SLOW CONNECTION!! Even a fast one may take a minute to load!

This is the polar equivalent, with the same dare.

http://marsprogram.jpl.nasa.gov/odyssey/gallery/latestimages/latest2003/jul/20030724a-02.jpg