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 |
| 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 |
| Syrtis Major Planum Channel and Depression: ESP_018988_1980 ESP_042882_1980 (Interval in Earth days: 1861) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 17.54 | 76.5 | 0 | -26.9 | 48.6 | 42.2 |
| 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 |
| Linear Dunes and Sand Sheets in Herschel Crater: ESP_016916_1655 ESP_017417_1655 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.1 | 129. | 5.50 | 22.91 | 58.0 | 60.0 |
| Layered Bedrock near Oyama Crater: ESP_018820_2035 ESP_019664_2035 (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 | 23.40 | 341. | 16.2 | -9.56 | 45.5 | 53.5 |
| Glacier?: ESP_018857_2225 ESP_019358_2225 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 42.21 | 50.5 | -6.4 | 8.421 | 47.8 | 51.8 |
| Alluvial Fan in Far Western Terra Tyrrhena: ESP_018738_1585 ESP_019160_1585 (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 | -21.4 | 67.0 | 0.22 | -17.5 | 66.6 | 65.9 |
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