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.
Western Rim and Ejecta of Mojave Crater: PSP_007494_1875 PSP_007850_1875 (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 | 7.410 | 326. | 8.05 | -4.28 | 42.0 | 45.7 |
Upper Section of Northern Olympus Mons Basal Scarp: PSP_007445_2035 PSP_008447_2035 (Interval in Earth days: 78) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.90 | 223. | -1.4 | -13.8 | 40.1 | 44.4 |
Light-Toned Rock Exposures: PSP_007101_1730 ESP_019311_1730 (Interval in Earth days: 952) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.99 | 260. | -7.9 | 3.361 | 44.7 | 56.7 |
Craters on an Ice-Rich Debris Apron: PSP_007832_1385 ESP_060736_1385 (Interval in Earth days: 4123) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -41.3 | 103. | 1.98 | -19.2 | 74.9 | 74.8 |
Line of Cones and Associated Flows in Arsia Sulci: PSP_007603_1770 ESP_036718_1770 (Interval in Earth days: 2269) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.83 | 231. | 8.18 | -17.6 | 47.1 | 57.8 |
Gullies Possibly Produced by Snow or Ice Melting: PSP_007270_2240 PSP_010487_2240 (Interval in Earth days: 251) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 43.42 | 319. | -2.8 | 11.76 | 45.5 | 52.4 |
Southern Branch of Kasei Valles: PSP_007891_1980 ESP_036162_1980 (Interval in Earth days: 2203) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.93 | 285. | -6.1 | 8.571 | 42.8 | 47.1 |
Flow-Banded Deformed Terrain of Hellas Basin Floor: PSP_007201_1405 PSP_007491_1405 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.9 | 54.9 | -7.0 | 3.906 | 65.3 | 68.9 |
Clinoforms in Melas Chasma: PSP_007878_1700 PSP_008735_1700 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.75 | 283. | 4.89 | -23.0 | 53.8 | 61.4 |
Well-Exposed Central Uplift in Unnamed Crater: PSP_007109_1555 ESP_019385_1555 (Interval in Earth days: 956) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -24.2 | 43.4 | 7.44 | -4.41 | 53.1 | 65.2 |
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