THE IMAGER FOR MARS PATHFINDER EXPERIMENT

Citation
Ph. Smith et al., THE IMAGER FOR MARS PATHFINDER EXPERIMENT, J GEO R-PLA, 102(E2), 1997, pp. 4003-4025
Citations number
38
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
ISSN journal
21699097 → ACNP
Volume
102
Issue
E2
Year of publication
1997
Pages
4003 - 4025
Database
ISI
SICI code
2169-9097(1997)102:E2<4003:TIFMPE>2.0.ZU;2-X
Abstract
The imager for Mars Pathfinder (IMP), a stereoscopic, multispectral ca mera, is described in terms of its capabilities for studying the Marti an environment. The camera's two eyes, separated by 15.0 cm, provide t he camera with range-finding ability. Each eye illuminates half of a s ingle CCD detector with a field of view of 14.4 x 14.0 degrees and has 12 selectable filters. The f/18 optics have a large depth of field, a nd no focussing mechanism is required; a mechanical shutter is avoided by using the frame transfer capability of the 512 x 512 CCD. The reso lving power of the camera, 0.98 mrad/pixel, is approximately the same as the Viking Lander cameras; however, the signal-to-noise ratio for I MP greatly exceeds Viking, approaching 350. This feature along with th e stable calibration of the filters between 440 and 1000 nm distinguis hes IMP from Viking. Specially designed targets are positioned on the Lander; they provide information on the magnetic properties of wind-bl own dust, measure the wind vectors, and provide radiometric standard r eflectors for calibration. Also, eight low-transmission filters are in cluded for imaging the Sun directly at multiple wavelengths, giving IM P the ability to measure dust opacity and potentially the water vapor content. Several experiments beyond the requisite color panorama are d escribed in detail: contour mapping of the local terrain, multispectra l imaging of the surrounding rock and soil to study local mineralogy, viewing of three wind socks, measuring atmospheric opacity and water v apor content, and estimating the magnetic properties of wind-blown dus t. This paper is intended to serve as a guide to understanding the sci entific integrity of the IMP data that will be returned from Mars star ting on July 4, 1997.