page_title: Thermal Emission Imaging System
section_title: Infrared camera
hierarchical_section_title: Thermal Emission Imaging System / Infrared camera
caption_attribution_description: English: Image of Saline Valley, California, taken by the Terra satellite's ASTER instrument.
context_page_description: The Thermal Emission Imaging System is a camera on board the 2001 Mars Odyssey orbiter. It images Mars in the visible and infrared parts of the electromagnetic spectrum in order to determine the thermal properties of the surface and to refine the distribution of minerals on the surface of Mars as determined by the Thermal Emission Spectrometer. Additionally, it helps scientists to understand how the mineralogy of Mars relates to its landforms, and it can be used to search for thermal hotspots in the Martian subsurface.
  THEMIS is managed from the Mars Space Flight Facility at Arizona State University and was built by the Santa Barbara Remote Sensing division of Raytheon. The instrument was named after the Greek goddess of justice.
context_section_description: THEMIS detects thermal infrared energy emitted by the Martian surface at nine different wavelengths.  Eight of these have wavelengths between 6 and 13 micrometers, an ideal region of the infrared spectrum to determine thermal energy patterns characteristic  of silicate minerals. The ninth band is at 14.9 micrometers and is used to monitor the Martian atmosphere.  The shortest infrared wavelength, at 6.78 micrometers, is measured twice in two bands to improve the signal-to-noise ratio.  THEMIS is therefore a 10-band instrument that detects nine different wavelengths .
  The absorption spectrum measured by THEMIS contains two kinds of information: temperature and emissivity.  The temperature contribution to the measurement dominates the spectrum unless the data is corrected.  In effect, a THEMIS infrared image taken during the day will look much like a shaded relief map, with slopes facing the sun being bright (hot) and shaded areas being dark (cold).  In a THEMIS image taken at night, however, thermophysical properties of the surface can be inferred, such as temperature differences due to the materials' grain size (thermal inertia).
  The effect of temperature can be removed from THEMIS infrared data by dividing the image by a black body curve.  The resulting energy pattern is an emissivity spectrum characteristic of the specific minerals (or other things) found on the surface.  The presence of minerals such as carbonates, silicates, hydroxides, sulfates, amorphous silica, oxides, and phosphates can be determined from THEMIS measurements.
  In particular, this multi-spectral method allows researchers to detect the presence of minerals that form in water and to understand those minerals in their geological context.
  The THEMIS infrared camera was designed to be used in conjunction with data from the Thermal Emission Spectrometer (TES), a similar instrument on Mars Global Surveyor.  While THEMIS has a very high spatial resolution (100 m) with a low spectral resolution of only 10 bands between 6 and 15 micrometers, TES has a low spatial resolution (3×6 km) with very high spectral resolution of 143 bands between 5 and 50 micrometers.
  
  The instrument's approach provides data on localized deposits associated with volcanoes, hydrothermal processes, and the alteration of minerals by surface and/or subsurface water.
  The Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), an Earth orbiting instrument on the Terra spacecraft, has used a similar approach to map the distribution of minerals on Earth.  Variations in the thermal infrared false-color image are due to differences in the minerals that make up rocks and soil.
caption: Sample map from Terra's ASTER instrument: Saline Valley, California
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