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.
| Landforms East of Sinai Planum: ESP_085667_1665 ESP_093855_1665 (Interval in Earth days: 638) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.4 | 282. | -8.2 | 10.72 | 39.4 | 33.4 |
| Margin of Athabasca Valles Lava: ESP_085672_1835 ESP_085738_1835 (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 | 3.686 | 142. | 7.88 | -7.30 | 36.3 | 37.7 |
| Landforms above Subsurface Radar Observations of South Polar Cap: ESP_085526_1000 ESP_085513_1000 (Interval in Earth days: 1) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -79.7 | 185. | 8.77 | -3.25 | 79.0 | 79.5 |
| Inverted Channel in Noachis Terra Displaying Morphological Change: ESP_085572_1440 ESP_085506_1440 (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 | -35.7 | 358. | -7.2 | 7.596 | 48.5 | 46.6 |
| Landform and Dunes in Arabia Terra: ESP_085625_1910 ESP_085836_1910 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.95 | 345. | -6.7 | 2.615 | 38.8 | 38.0 |
| Fissure in Athabasca Valles: ESP_085500_1900 ESP_085711_1900 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.733 | 156. | 1.29 | 15.59 | 38.1 | 36.6 |
| North Pole Facing Deposit in Crater: ESP_085325_2220 ESP_085813_2220 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 41.70 | 249. | -2.3 | 2.947 | 58.0 | 51.8 |
| Transect of Ladon Valles: ESP_085441_1560 ESP_085507_1560 (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 | -23.7 | 330. | 9.97 | -6.87 | 39.3 | 41.3 |
| Stepped Features in Tartarus Skopulus: ESP_085684_1800 ESP_085829_1800 (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 | 0.074 | 175. | 2.52 | 26.97 | 36.6 | 35.2 |
| Eroded Layered Bedrock: ESP_085567_1555 ESP_085923_1555 (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 | -24.3 | 132. | -6.1 | 16.95 | 42.3 | 45.7 |
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