The DOI matches its Crossref record; 37 of the 37 references it cites were found in a registry or an index.
Mars Observer camera
Open accessAbstract
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 × 2.8 km to 2.8 km × 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 × 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.
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Citations
Cites
Wind as a Geological Process: On Earth, Mars, Venus and Titan
Greeley, R., & Iversen, J. D. (1985) · Cambridge University Press eBooks · doi:10.1017/cbo9780511573071 · Cited by 688
Properties and effects of dust particles suspended in the Martian atmosphere
Pollack, J. B., Colburn, D. S., Flasar, F. M., Kahn, R., Carlston, C. E., & Pidek, D. (1979) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb084ib06p02929 · Cited by 578
Formation of Martian flood features by release of water from confined aquifers
Carr, M. H. (1979) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb084ib06p02995 · Cited by 524
The astronomical theory of climatic change on Mars
Toon, O. B., Pollack, J. B., Ward, W., Burns, J. A., & Bilski, K. (1980) · Icarus · doi:10.1016/0019-1035(80)90130-x · Cited by 351
Martian impact craters and emplacement of ejecta by surface flow
Carr, M. H., Crumpler, L. S., Cutts, J. A., Greeley, R., Guest, J. E., & Masursky, H. (1977) · Journal of Geophysical Research · doi:10.1029/js082i028p04055 · Cited by 317
Self-citationSHARP, R. P., & MALIN, M. C. (1975) · Geological Society of America Bulletin · doi:10.1130/0016-7606(1975)86<593:com>2.0.co;2 · Cited by 311
Self-citationSome Martian volcanic features as viewed from the Viking orbiters
Carr, M. H., Greeley, R., Blasius, K. R., Guest, J. E., & Murray, J. B. (1977) · Journal of Geophysical Research · doi:10.1029/js082i028p03985 · Cited by 261
Martian Valleys: Morphology, Distribution, Age, and Origin
Pieri, D. C. (1980) · Science · doi:10.1126/science.210.4472.895 · Cited by 255
Carr, M. H. (1973) · Journal of Geophysical Research · doi:10.1029/jb078i020p04049 · Cited by 252
Water and processes of degradation in the Martian landscape
Milton, D. J. (1973) · Journal of Geophysical Research · doi:10.1029/jb078i020p04037 · Cited by 241
Cited by
Evidence for Recent Groundwater Seepage and Surface Runoff on Mars
Malin, M. C., & Edgett, K. S. (2000) · Science · doi:10.1126/science.288.5475.2330 · Cited by 1,082
Self-citationSedimentary rocks of early Mars
Malin, M. C., & Edgett, K. S. (2000) · Science · doi:10.1126/science.290.5498.1927 · Cited by 842
Self-citationGeologic context of proposed chloride‐bearing materials on Mars
Osterloo, M. M., Anderson, F. S., Hamilton, V. E., & Hynek, B. M. (2010) · Journal of Geophysical Research: Planets · doi:10.1029/2010je003613 · Cited by 274
Voluminous volcanism on early Mars revealed in Valles Marineris
McEwen, A. S., Malin, M. C., Carr, M. H., & Hartmann, W. K. (1999) · Nature · doi:10.1038/17539 · Cited by 259
Self-citationLiu, J., Richardson, M. I., & Wilson, R. J. (2003) · Journal of Geophysical Research: Planets · doi:10.1029/2002je001921 · Cited by 112
Metadata
- Authors
- Malin, M. C., Danielson, G. E., Ingersoll, A. P., Masursky, H., Veverka, J., Ravine, M. A., & Soulanille, T. A.
- Venue
- Journal of Geophysical Research: Planets
- Publisher
- American Geophysical Union (AGU)
- Published
- 1992-05-25
- Volume
- 97
- Issue
- E5
- Pages
- 7699-7718
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W1618627478
- Cited by
- 277
- References
- 37
- FWCI
- 2.62
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Malin, M. C., Danielson, G. E., Ingersoll, A. P., Masursky, H., Veverka, J., Ravine, M. A., & Soulanille, T. A. (1992). Mars Observer camera. Journal of Geophysical Research: Planets. https://doi.org/10.1029/92je00340
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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