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.
| Dune Changes in Green Crater: ESP_023145_1270 ESP_022855_1270 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -52.6 | 351. | 20.8 | -0.20 | 45.6 | 43.7 |
| Proposed Landing Site in Mawrth Vallis: ESP_023488_2050 ESP_023554_2050 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.53 | 338. | 6.73 | -14.0 | 44.9 | 45.5 |
| Clay-Bearing Layered Deposit in Unnamed Crater North of Proctor Crater: ESP_023302_1345 ESP_023803_1345 (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 | -45.3 | 27.9 | -8.6 | 6.167 | 44.4 | 51.2 |
| Craters in South Polar Layered Material: ESP_023364_1045 ESP_023469_1045 (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 | -75.2 | 148. | -14. | 27.20 | 68.5 | 68.0 |
| Light-Toned Material in Noctis Region Fracture: ESP_023214_1695 ESP_023926_1695 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.2 | 264. | 3.07 | 19.20 | 31.5 | 33.2 |
| Changes in Intracrater Dunes: ESP_023186_1765 ESP_023463_1765 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -3.28 | 307. | 4.33 | -23.3 | 33.1 | 34.3 |
| Gully Change Detection: ESP_023111_1330 ESP_023032_1330 (Interval in Earth days: 6) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -46.3 | 197. | 29.0 | 2.043 | 40.3 | 41.2 |
| Light-Toned Phyllosilicates along Plains at Coprates Catena: ESP_023160_1650 ESP_024017_1650 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.8 | 301. | -25. | 8.371 | 33.5 | 36.4 |
| South Polar Layered Material along Crater Rim: ESP_023377_1050 ESP_032067_1050 (Interval in Earth days: 677) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -75.0 | 146. | 7.29 | -6.93 | 67.3 | 66.2 |
| Ultimum Chasma South Polar Layers: ESP_023456_0990 ESP_041100_0990 (Interval in Earth days: 1375) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -80.7 | 155. | 7.58 | -6.73 | 73.4 | 74.7 |
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