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.
Contact between Polygon and Massif: PSP_005700_2200 ESP_011818_2200 (Interval in Earth days: 477) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.77 | 346. | 0 | -24.3 | 59.2 | 72.7 |
Polar Layered Deposit Stratigraphy Near Chasma Australe: PSP_004840_0940 PSP_005078_0940 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.1 | 94.2 | 20.6 | 6.758 | 64.4 | 67.7 |
Lobate Crater Ejecta: PSP_005867_1330 ESP_011431_1330 (Interval in Earth days: 434) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -46.4 | 118. | 0 | 14.15 | 48.3 | 67.4 |
Streamlined Hills in the Western Charitum Montes: PSP_006902_1275 ESP_011398_1275 (Interval in Earth days: 350) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -52.1 | 301. | -7.0 | 7.062 | 70.2 | 70.9 |
Light-Toned Layered Rock Outcrop in Hellas Region: PSP_006700_1385 ESP_016141_1385 (Interval in Earth days: 736) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -41.1 | 53.1 | 5.27 | -12.5 | 58.1 | 68.9 |
Light-Toned Layered Rock Outcrop in Ladon Vallis: PSP_006637_1590 ESP_023383_1590 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -20.8 | 330. | 7.10 | 20.68 | 44.1 | 31.2 |
Mawrth Vallis Phillosilicate Layers: PSP_005819_2050 PSP_006742_2050 (Interval in Earth days: 72) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 24.68 | 339. | 3.35 | -7.74 | 46.6 | 40.7 |
Layered Bedrock Exposed in the Central Uplift of Martin Crater: PSP_005610_1585 PSP_005887_1585 (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 | -21.4 | 290. | 1.73 | -24.8 | 33.4 | 37.3 |
Seasonal Monitoring: PSP_005340_0930 PSP_005523_0930 (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 | -87.0 | 170. | 0.24 | 20.31 | 72.8 | 73.3 |
Exposure of South Polar Layered Deposits: PSP_004994_1040 PSP_005297_1040 (Interval in Earth days: 24) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -75.7 | 201. | 2.74 | 25.62 | 58.6 | 60.5 |
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