MARS-OBSERVER CAMERA

被引:230
作者
MALIN, MC
DANIELSON, GE
INGERSOLL, AP
MASURSKY, H
VEVERKA, J
RAVINE, MA
SOULANILLE, TA
机构
[1] ARIZONA STATE UNIV, DEPT GEOL, TEMPE, AZ 85287 USA
[2] CALTECH, DIV GEOPHYS & PLANETARY SCI, PASADENA, CA 91125 USA
[3] US GEOL SURVEY, ASTROGEOL BRANCH, FLAGSTAFF, AZ 86001 USA
[4] CORNELL UNIV, CTR RADIOPHYS & SPACE PHYS, ITHACA, NY 14853 USA
[5] ALTADENA INSTRUMENTS CORP, PASADENA, CA USA
关键词
D O I
10.1029/92JE00340
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 Mars Observer camera (MOC) is a three-component system (one narrow-angle and two wide-angle cameras) designed to take high spatial resolution pictures of the surface of Mars and to obtain lower spatial resolution, synoptic coverage of the planet's surface and atmosphere. The cameras are based on the ''push broom'' technique; that is, they do not take ''frames'' but rather build pictures, one line at a time, as the spacecraft moves around the planet in its orbit. MOC is primarily a telescope for taking extremely high resolution pictures of selected locations on Mars. Using the narrow-angle camera, areas ranging from 2.8 km x 2.8 km to 2.8 km x 25.2 km (depending on available internal digital buffer memory) can be photographed at about 1.4 m/pixel. Additionally, lower-resolution pictures (to a lowest resolution of about 11 m/pixel) can be acquired by pixel averaging: these images can be much longer, ranging up to 2.8 x 500 km at 11 m/pixel. High-resolution data will be used to study sediments and sedimentary processes, polar processes and deposits, volcanism, and other geologic/geomorphic processes. The MOC wide-angle cameras are capable of viewing Mars from horizon to horizon and are designed for low-resolution global and intermediate resolution regional studies. Low-resolution observations can be made every orbit, so that in a single 24-hour period a complete global picture of the planet can be assembled at a resolution of at least 7.5 km/pixel. Regional areas (covering hundreds of kilometers on a side) may be photographed at a resolution of better than 250 m/pixel at the nadir. Such images will be particularly useful in studying time-variable features such as lee clouds, the polar cap edge, and wind streaks, as well as acquiring stereoscopic coverage of areas of geological interest. The limb can be imaged at a vertical and along-track resolution of better than 1.5 km. Different color filters within the two wide-angle cameras permit color images of the surface and atmosphere to be made to distinguish between clouds and the ground and between clouds of different composition.
引用
收藏
页码:7699 / 7718
页数:20
相关论文
共 62 条
[1]  
ALBEE AL, 1992, J GEOPHYS RES, V97
[2]  
Baker V.R, 1982, THE CHANNELS OF MARS, P198, DOI DOI 10.1029/EO063I045P00862
[3]   PALEOHYDRAULIC INTERPRETATION OF QUATERNARY ALLUVIUM NEAR GOLDEN, COLORADO [J].
BAKER, VR .
QUATERNARY RESEARCH, 1974, 4 (01) :94-112
[4]  
BELTON MJS, 1976, J ATMOS SCI, V33, P1394, DOI 10.1175/1520-0469(1976)033<1394:CPWACI>2.0.CO
[5]  
2
[6]  
Blasius K. R., 1977, Journal of Geophysical Research, V82, P4067, DOI 10.1029/JS082i028p04067
[7]  
BRIGGS G, 1976, J GEOPHYS RES, V82, P4121
[8]   VIKING ORBITER IMAGING OBSERVATIONS OF DUST IN THE MARTIAN ATMOSPHERE [J].
BRIGGS, GA ;
BAUM, WA ;
BARNES, J .
JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB6) :2795-2820
[9]  
Carr M. H., 1977, Journal of Geophysical Research, V82, P4055, DOI 10.1029/JS082i028p04055
[10]  
Carr M. H., 1977, Journal of Geophysical Research, V82, P3985, DOI 10.1029/JS082i028p03985