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Journal ArticleDOI

The Mars Observer laser altimeter investigation

TLDR
The Mars Observer laser altimeter (MOLA) was used to determine globally the topography of Mars at a level suitable for addressing problems in geology and geophysics as mentioned in this paper.
Abstract
The primary objective of the Mars Observer laser altimeter (MOLA) investigation is to determine globally the topography of Mars at a level suitable for addressing problems in geology and geophysics. Secondary objectives are to characterize the 1064-nm wavelength surface reflectivity of Mars to contribute to analyses of global surface mineralogy and seasonal albedo changes, to assist in addressing problems in atmospheric circulation, and to provide geodetic control and topographic context for the assessment of possible future Mars landing sites. The principal components of MOLA are a diode-pumped, neodymium-doped yttrium aluminum garnet laser transmitter that emits 1064-nm wavelength laser pulses, a 0.5-m-diameter telescope, a silicon avalanche photodiode detector, and a time interval unit with 10-ns resolution. MOLA will provide measurements of the topography of Mars within approximately 160-m footprints and a center-to-center along-track foot print spacing of 300 m along the Mars Observer subspacecraft ground track. The elevation measurements will be quantized with 1.5 m vertical resolution before correction for orbit- and pointing induced errors. MOLA profiles will be assembled into a global 0.2 deg x 0.2 deg grid that will be referenced to Mars' center of mass with an absolute accuracy of approximately 30 m. Other data products will include a global grid of topographic gradients, corrected individual profiles, and a global 0.2 deg x 0.2 deg grid of 1064-nm surface reflectivity.

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Coastal Geomorphology of the Martian northern plains

TL;DR: Parker et al. as mentioned in this paper considered the formation of the outflow channels and valley networks discovered on the Martian northern plains during the Mariner 9 mission and suggested that geological processes capable of producing similar morphologies on earth, lacustrine or marine deposition and subsequent periglacial modification offer the simplest and most consistent explanation for the suit of features found on Mars.
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Chloride-Bearing Materials in the Southern Highlands of Mars

TL;DR: The identification of chlorides in the ancient southern highlands suggests that near-surface water was available and widespread in early Martian history.
References
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Journal ArticleDOI

Ascent and eruption of basaltic magma on the earth and moon

TL;DR: In this paper, the ascent and emplacement of basaltic magma on the earth and moon is modeled by the application of geological and physical observations and constraints, provided that allowance is made for the coalescence of gas bubbles.
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The Influence of Gravity Wave Breaking on the General Circulation of the Middle Atmosphere

TL;DR: In this article, the zonal mean solstice circulation of the global middle atmosphere is simulated using a semi-spectral numerical model, and it is shown that gravity wave drag and diffusion in the mesosphere can account for the observed large departure from radiative equilibrium in both summer and winter.
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Properties and effects of dust particles suspended in the Martian atmosphere

TL;DR: In this paper, the authors measured the optical depth above the two Viking landers for a period covering the summer, fall, and winter seasons in the Northern Hemisphere, a time period during which two global dust storms occurred.
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Flexural rigidity, thickness, and viscosity of the lithosphere

TL;DR: In this article, the flexural rigidity of the earth's lithosphere is deduced from observations of the wavelength and amplitude of bending in the vicinity of supercrustal loads.
Journal ArticleDOI

Formation of Martian flood features by release of water from confined aquifers

TL;DR: In this paper, it is proposed that the rapid release of water under great pressure from deeply buried aquifers is responsible for the formation of the Martian channels suggestive of catastrophic flooding (outflow channels).
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