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.
| Dunes on Cemented Substrate: ESP_019130_2600 ESP_019157_2600 (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 | 79.98 | 122. | 27.5 | 2.09 | 64.3 | 66.1 |
| Pits North of Alba Patera: ESP_018955_2310 ESP_018256_2310 (Interval in Earth days: 54) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 50.63 | 254. | -14. | 11.85 | 51.4 | 43.8 |
| North Polar Layered Deposits: ESP_018961_2670 ESP_019145_2670 (Interval in Earth days: 15) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 86.71 | 73.6 | -18. | -9.58 | 68.9 | 70.7 |
| Change Detection in Aeolis Planum: ESP_019038_1740 ESP_019882_1740 (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 | -6.07 | 153. | 9.19 | -15.2 | 56.3 | 56.9 |
| Steep North-Polar Boundary Scarp: ESP_018905_2650 ESP_019222_2650 (Interval in Earth days: 25) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.99 | 151. | -3.6 | -15.5 | 66.5 | 71.1 |
| Possible Fluvial Features in West Hellas Planitia: ESP_019042_1450 ESP_019187_1450 (Interval in Earth days: 11) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -34.8 | 48.5 | 4.88 | 17.60 | 73.2 | 71.3 |
| Exposure of Polar Layered Deposits: ESP_019069_2680 ESP_018108_2680 (Interval in Earth days: 75) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.05 | 329. | -11. | -23.0 | 70.9 | 63.9 |
| Layered Rocks and Scarp on Crater Floor: ESP_019024_1930 ESP_037577_1930 (Interval in Earth days: 1446) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 13.04 | 174. | -6.3 | 15.43 | 50.3 | 54.4 |
| Possible Future Landing Site in Antoniadi Crater: ESP_018883_2010 ESP_019305_2010 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.51 | 63.0 | -1.7 | -16.7 | 47.8 | 51.3 |
| Eberswalde Crater Deposits: ESP_019190_1560 ESP_019335_1560 (Interval in Earth days: 12) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.9 | 326. | 0.12 | 15.06 | 65.9 | 64.0 |
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