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.
| Bedform Migration Near Chasma Boreale: ESP_027627_2645 ESP_027654_2645 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.38 | 343. | 7.02 | -7.90 | 64.5 | 65.5 |
| Small Crater on North Polar Deposits: ESP_027492_2615 ESP_027874_2615 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 81.32 | 91.4 | -6.4 | 11.96 | 61.8 | 64.9 |
| Candidate Future Landing Site in Elysium Planitia: ESP_027702_1815 ESP_026792_1815 (Interval in Earth days: 71) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 1.616 | 138. | -0.1 | 20.11 | 52.8 | 50.8 |
| Crater in Meridiani Planum: ESP_027694_1815 ESP_045074_1815 (Interval in Earth days: 1354) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 0.767 | 355. | 19.3 | 9.447 | 51.8 | 50.0 |
| Change Detection in Barchan Dune Source: ESP_027746_2650 ESP_027628_2650 (Interval in Earth days: 9) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.93 | 331. | 6.25 | -8.54 | 66.2 | 65.6 |
| Light-Toned Layered Deposits in Ladon Valles: ESP_027471_1600 ESP_027537_1600 (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 | -19.9 | 327. | -8.1 | -26.1 | 65.5 | 66.6 |
| Layered Blocks Leaning against Slopes in Deuteronilus Mensae: ESP_027574_2245 ESP_028339_2245 (Interval in Earth days: 59) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 44.05 | 26.1 | 6.68 | -15.5 | 45.5 | 55.9 |
| North Polar Dunes: ESP_027529_2620 ESP_027344_2620 (Interval in Earth days: 14) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 81.85 | 160. | -5.2 | 8.882 | 62.5 | 60.2 |
| Complex Superposition of Fractures: ESP_027618_2235 ESP_027974_2235 (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 | 43.02 | 268. | -17. | 0.935 | 47.7 | 49.6 |
| Layers in Western Arabia Region Crater: ESP_027615_1880 ESP_060331_1880 (Interval in Earth days: 2549) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 7.825 | 352. | 0 | -14.8 | 50.2 | 40.7 |
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