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.
| Giza Region Unfrosted: PSP_004736_0950 PSP_005119_0950 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -84.8 | 65.7 | 1.48 | -14.5 | 64.0 | 68.7 |
| Ridges in Nili Fossae Phyllosilicates: PSP_005855_2020 PSP_006712_2020 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 21.80 | 77.1 | -2.4 | 7.233 | 44.7 | 38.7 |
| Streamlined Features in Argyre Planitia: PSP_006163_1345 ESP_011714_1345 (Interval in Earth days: 433) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -45.3 | 316. | 0 | -23.3 | 52.2 | 65.7 |
| 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 |
| Exposure of High-Latitude Polar Layered Deposits Not Well Observed: PSP_005971_0890 PSP_005957_0910 (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 | -88.7 | 251. | 18.6 | 19.51 | 83.1 | 82.5 |
| Young Double-Layer Ejecta Crater: PSP_006816_2120 PSP_007027_2120 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 31.47 | 116. | 5.98 | -4.03 | 42.0 | 41.9 |
| Deeply-Penetrating Structure within Polar Layered Deposits: PSP_005076_0940 PSP_005207_0940 (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 | -86.1 | 172. | -8.4 | 5.833 | 69.3 | 69.2 |
| Light-Toned Layering on Plains Next to Ganges Chasma: PSP_005161_1720 ESP_016237_1720 (Interval in Earth days: 863) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.14 | 307. | 6.27 | -10.6 | 35.3 | 48.9 |
| Hanging Valley in Minio Vallis: PSP_006470_1760 PSP_007762_1760 (Interval in Earth days: 101) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.14 | 208. | 0 | 23.15 | 36.5 | 48.2 |
| Valley Network along Melas Chasma Wallrock: PSP_005663_1700 ESP_012493_1700 (Interval in Earth days: 532) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.67 | 282. | -4.4 | -21.3 | 33.4 | 54.0 |
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