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.
| Evolution of Surface Near the Granicus and Tinjar Valles: PSP_005932_2080 ESP_057873_2080 (Interval in Earth days: 4047) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 27.73 | 135. | -18. | 2.277 | 48.7 | 58.1 |
| Fresh Crater: PSP_005517_2240 PSP_005807_2240 (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 | 43.80 | 301. | -0.2 | 20.25 | 65.1 | 59.8 |
| 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 |
| 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 |
| Possible Exposure of Polar Layered Deposits in Area Not Well Observed: PSP_004882_0880 PSP_004894_0920 (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 | -88.1 | 121. | 11.7 | 11.47 | 68.6 | 67.9 |
| 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 |
| Large Region of Layering in Meridiani Planum: PSP_006227_1810 ESP_011791_1810 (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 | 1.126 | 2.68 | 0 | 28.55 | 34.9 | 55.4 |
| Thermally-Distinct Rays Emanating from Gratteri Crater: PSP_006510_1635 ESP_020922_1635 (Interval in Earth days: 1123) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.3 | 197. | 0 | 27.48 | 40.6 | 49.7 |
| Southern Ejecta of Tooting Crater: PSP_006760_2035 PSP_007406_2035 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.10 | 207. | -7.0 | 6.07 | 40.1 | 39.4 |
| Layers at the Head of Chasma Australe Exposed over 270 Degrees of Azimuth: PSP_004788_0945 PSP_005079_0945 (Interval in Earth days: 23) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.6 | 95.5 | 0 | -16.3 | 65.3 | 69.7 |
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