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.
| High-Latitude Exposure of North Polar Layered Deposits: ESP_019117_2720 ESP_019050_2720 (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 | 87.74 | 6.00 | -13. | -23.1 | 73.5 | 73.7 |
| Central Structure of Jorn Crater: ESP_019186_1525 ESP_025199_1525 (Interval in Earth days: 469) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.1 | 76.4 | 0 | -29.5 | 67.8 | 62.4 |
| Translucent Ice on Dunes: ESP_019006_2550 ESP_019243_2550 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 74.97 | 300. | -21. | 3.245 | 63.1 | 64.3 |
| Gemina Lingula Scarp with Outcrop of Layered Deposits and Unconformities: ESP_018844_2605 ESP_019081_2605 (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 | 80.37 | 27.0 | 1.70 | 16.54 | 62.6 | 64.5 |
| Steep North Polar Boundary Scarp: ESP_018943_2655 ESP_019181_2655 (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 | 85.36 | 186. | 0 | -13.2 | 67.0 | 70.6 |
| Well-Preserved Impact Crater in Arabia Terra: ESP_019162_1975 ESP_019439_1975 (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 | 17.23 | 5.48 | 7.48 | -19.6 | 48.9 | 52.7 |
| Steep North-Polar Boundary Scarp: ESP_018957_2655 ESP_019195_2655 (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 | 85.25 | 160. | 3.29 | -9.91 | 67.0 | 70.5 |
| 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 |
| Cluster of Zunil Crater Secondaries: ESP_019064_1835 ESP_019209_1835 (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 | 3.656 | 163. | 2.92 | 17.53 | 52.6 | 51.6 |
| 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 |
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