Planned stereo pairs have suitable stereo convergence angles and illumination by design.
In addition to planned stereo pairs, the Pairendipity software can identify overlapping
HiRISE images that are serendipitously suitable for stereo processing and find stereo
pairs within the CTX dataset.
Planned HiRISE stereo pairs are listed in the “Stereo Pair List (CSV)” link below.
Since this list is based on produced stereo anaglyphs it also contains a few serendipitous
pairs that underwent special processing. Most serendipitous HiRISE stereo pairs are listed
in the “Pairendipity Stereo” link, while CTX stereo pairs are listed
in “Pairendipity CTX Stereo”.
Images taken close together in time minimize illumination and frost differences and are
especially useful (see the Delta-Days column in the Pairendipity files or difference
the orbit numbers in the image IDs in the Stereo Pair List file). Stereo pairs
with both images planned within the same 14-day (168-orbit) operations cycle are known as SPORCs.
High-Latitude Exposure of North Polar Layered Deposits: PSP_009187_2680 ESP_018221_2680 (Interval in Earth days: 704) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.92 | 95.3 | -6.5 | -14.0 | 63.1 | 63.7 |
Central Peak and Floor of Large Crater West of Schiaparelli Crater: PSP_008613_1760 PSP_008969_1760 (Interval in Earth days: 28) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -3.93 | 12.2 | 1.91 | -18.6 | 55.6 | 58.3 |
Well-Preserved 9-Kilometer Diameter Crater: PSP_008902_1565 PSP_009680_1565 (Interval in Earth days: 60) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.0 | 43.1 | -5.5 | -19.4 | 69.6 | 70.5 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_009263_2675 PSP_009370_2675 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.49 | 182. | -3.5 | -13.3 | 62.9 | 63.2 |
Basal Units in North Polar Region: PSP_009134_2645 PSP_009687_2645 (Interval in Earth days: 43) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.66 | 157. | -7.5 | 10.32 | 60.3 | 62.1 |
Pits along the Claritas Rupes: PSP_008512_1630 PSP_009013_1630 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.6 | 251. | 6.29 | -8.58 | 62.9 | 65.6 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_009243_2675 PSP_009297_2675 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 87.62 | 13.0 | -5.1 | -13.9 | 62.9 | 63.0 |
Mid-Latitude Crater with Gullied Central Structure and South-Facing Slopes: PSP_009298_2295 ESP_025082_2295 (Interval in Earth days: 1229) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 49.13 | 21.0 | -0.2 | -23.2 | 44.7 | 47.7 |
Flows on the Northeastern Flank of Arsia Mons: PSP_008565_1720 PSP_009844_1720 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.68 | 242. | 9.15 | -10.2 | 57.2 | 60.4 |
Key Contact Relationships and Morphologic Correlations: PSP_009279_2650 PSP_009451_2650 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.69 | 156. | -5.6 | -19.3 | 60.6 | 62.2 |
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