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Radiometry Measurements of Mars at 1064 nm Using the Mars Orbiter Laser AltimeterMeasurements by the Mars Orbiter Laser Altimeter (MOLA) on board the Mars Global Surveyor (MGS) may be used to provides a radiometric measurement of Mars in addition to the topographic measurement. We will describe the principle of operation, a mathematical model, and the receiver calibration in this presentation. MOLA was designed primarily to measure Mars topography, surface roughness end the bidirectional reflectance to the laser beam. To achieve the highest sensitivity the receiver detection threshold is dynamically adjusted to be as low as possible while keeping a predetermined false alarm rate. The average false alarm rate 29 monitored in real time on board MOLA via a noise counter, whose output is fed to the threshold control loop. The false alarm rate at a given threshold is a function of the detector output noise which is the sum of the photo detector, shot noise due to the background light seen by the detector and the dark noise. A mathematical model has been developed that can be used to numerically solve for the optical background power given the MOLA threshold setting and the average noise count. The radiance of Mars can then be determined by dividing the optical power by the solid angle subtended by the MOLA receiver, the receiver optical band-width, end the Mars surface area within the receiver field of view. The phase angle which is the sun-Mars-MOLA angle is available from the MGS database. MOLA also measures simultaneously the bidirectional reflectance of Mars vie its 106-lum loser beam at nadir with nearly zero phase angle. The optical bandwidth of the MOLA receiver is 2um full width at half maximum (FWHM) and centered at 106-lum. The receiver field of view is 0.95mrad FWHM. The nominated spacecraft altitude is 100km and the ground track speed is about 3km/s. Under normal operation, the noise counter are read and the threshold levels are updated at 1Hz. The receiver sensitivity is limited by the detector dark noise to about 0.1nW, which corresponds to less than 2% the maximum radiance during daytime from the brightest area on Mars. The results from the mathematical model agree well with the prelaunch measurements at several calibrated optical power levels. The radiance of sunlit Mars estimated with this technique correlates well with the measurement from the MGS. Thermal Emission Spectrometer (TES) and the Hubble Space Telescope at similar wavelength.
Document ID
20020021948
Acquisition Source
Goddard Space Flight Center
Document Type
Conference Paper
Authors
Sun, Xiao-Li
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Abshire, James B.
(NASA Goddard Space Flight Center Greenbelt, MD United States)
Neumann, Gregory A.
(Massachusetts Inst. of Tech. Cambridge, MA United States)
Zuber, Maria T.
(Massachusetts Inst. of Tech. Cambridge, MA United States)
Smith, David E.
Date Acquired
August 20, 2013
Publication Date
January 1, 2001
Subject Category
Lunar And Planetary Science And Exploration
Meeting Information
Meeting: 2001 American Geophysical Union Fall Meeting
Location: San Francisco, CA
Country: United States
Start Date: December 10, 2001
End Date: December 14, 2001
Sponsors: American Geophysical Union
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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