File:PIA19816-Mars-EstimatingCarbon-Orbiters-20150902.jpg

Page contents not supported in other languages.
This is a file from the Wikimedia Commons
From Wikipedia, the free encyclopedia

Original file(1,234 × 616 pixels, file size: 68 KB, MIME type: image/jpeg)

Summary

Description
English: PIA19816: Multiple Instruments Used for Mars Carbon Estimate

http://photojournal.jpl.nasa.gov/catalog/PIA19816

IMAGE:

http://photojournal.jpl.nasa.gov/jpeg/PIA19816.jpg

ANNOTATED IMAGE:

http://photojournal.jpl.nasa.gov/figures/PIA19816_fig1.jpg

Researchers estimating the amount of carbon held in the ground at the largest known carbonate-containing deposit on Mars utilized data from three different NASA Mars orbiters.

Each image in this pair covers the same area about 36 miles (58 kilometers) wide in the Nili Fossae plains region of Mars' northern hemisphere. The tally of carbon content in the rocks of this region is a key piece in solving a puzzle of how the Martian atmosphere has changed over time. Carbon dioxide from the atmosphere on early Mars reacted with surface rocks to form carbonate, thinning the atmosphere.

The image on the left presents data from the Thermal Emission Imaging System (THEMIS) instrument on NASA's Mars Odyssey orbiter. The color coding indicates thermal inertia -- the property of how quickly a surface material heats up or cools off. Sand, for example (blue hues), cools off quicker after sundown than bedrock (red hues) does.

The color coding in the image on the right presents data from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) instrument on NASA's Mars Reconnaissance Orbiter. From the brightness at many different wavelengths, CRISM data can indicate what minerals are present on the surface. In the color coding used here, green hues are consistent with carbonate-bearing materials, while brown or yellow hues are olivine-bearing sands and locations with purple hues are basaltic in composition. The gray scale base map is a mosaic of daytime THEMIS infrared images.

Annotations point to areas with different surface compositions. The scale bar indicates 20 kilometers (12.4 miles).

In addition to data from THEMIS and CRISM, researchers estimating the amount of carbon in rocks of the Nili Fossae plains used data from the Thermal Emission Spectrometer instrument on NASA's Mars Global Surveyor orbiter, which operated from 1997 to 2006, and from two telescopic cameras on Mars Reconnaissance Orbiter: the Context Camera and the High Resolution Imaging Science Experiment.

Arizona State University, Tempe, provided and operates THEMIS. The Johns Hopkins University Applied Physics Laboratory, Laurel, Maryland, provided and operates CRISM. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Mars Reconnaissance Orbiter and Mars Odyssey projects for NASA's Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, built the orbiters and collaborates with JPL to operate them.
Date
Source http://photojournal.jpl.nasa.gov/figures/PIA19816_fig1.jpg
Author NASA/JPL-Caltech/ASU/JHUAPL

Licensing

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
Warnings:

Captions

Add a one-line explanation of what this file represents

Items portrayed in this file

depicts

2 September 2015

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current23:19, 2 September 2015Thumbnail for version as of 23:19, 2 September 20151,234 × 616 (68 KB)DrbogdanUser created page with UploadWizard
The following pages on the English Wikipedia use this file (pages on other projects are not listed):

Global file usage

The following other wikis use this file: