THE MARS-OBSERVER LASER ALTIMETER INVESTIGATION

被引:440
作者
ZUBER, MT
SMITH, DE
SOLOMON, SC
MUHLEMAN, DO
HEAD, JW
GARVIN, JB
ABSHIRE, JB
BUFTON, JL
机构
[1] JOHNS HOPKINS UNIV, DEPT EARTH & PLANETARY SCI, BALTIMORE, MD 21218 USA
[2] MIT, DEPT EARTH ATMOSPHER & PLANETARY SCI, CAMBRIDGE, MA 02139 USA
[3] CALTECH, DIV GEOL & PLANETARY SCI, PASADENA, CA 91125 USA
[4] BROWN UNIV, DIV GEOL SCI, PROVIDENCE, RI 02912 USA
[5] NASA, GODDARD SPACE FLIGHT CTR, TERR PHYS LAB, GREENBELT, MD 20771 USA
关键词
D O I
10.1029/92JE00341
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 footprint 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-degrees x 0.2-degrees 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-degrees x 0.2-degrees grid of 1064-nm surface reflectivity.
引用
收藏
页码:7781 / 7797
页数:17
相关论文
共 110 条
[1]  
ALBEE AL, 1992, J GEOPHYS RES-PLANET, V97
[2]  
Baker V.R, 1982, THE CHANNELS OF MARS, P198, DOI DOI 10.1029/EO063I045P00862
[3]   EROSION BY CATASTROPHIC FLOODS ON MARS AND EARTH [J].
BAKER, VR ;
MILTON, DJ .
ICARUS, 1974, 23 (01) :27-41
[4]   GRAVITY-FIELD MODEL OF MARS IN SPHERICAL-HARMONICS UP TO DEGREE AND ORDER 18 [J].
BALMINO, G ;
MOYNOT, B ;
VALES, N .
JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB12) :9735-9746
[5]   THICK SHELL TECTONICS ON ONE-PLATE PLANETS - APPLICATIONS TO MARS [J].
BANERDT, WB ;
PHILLIPS, RJ ;
SLEEP, NH ;
SAUNDERS, RS .
JOURNAL OF GEOPHYSICAL RESEARCH, 1982, 87 (NB12) :9723-9733
[6]  
BANERDT WB, 1992, IN PRESS MARS
[7]   POSSIBLE EFFECTS OF BREAKING GRAVITY-WAVES ON THE CIRCULATION OF THE MIDDLE ATMOSPHERE OF MARS [J].
BARNES, JR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B2) :1401-1421
[8]   MARINER ULTRAVIOLET SPECTROMETER - TOPOGRAPHY AND POLAR CAP [J].
BARTH, CA ;
HORD, CW .
SCIENCE, 1971, 173 (3993) :197-+
[9]   MARS TOPOGRAPHY HARMONICS AND GEOPHYSICAL IMPLICATIONS [J].
BILLS, BG ;
FERRARI, AJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1978, 83 (NB7) :3497-3508
[10]   STUDY OF MARTIAN TOPOGRAPHY BY ANALYTIC PHOTOGRAMMETRY [J].
BLASIUS, KR .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (20) :4411-4423