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.
| Central Structure of Wahoo Crater: ESP_018214_2035 ESP_018847_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 | 23.26 | 326. | 10.4 | -8.96 | 43.9 | 47.8 |
| Pitted Terrain North of Hrad Vallis: ESP_018168_2160 ESP_019012_2160 (Interval in Earth days: 65) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.59 | 141. | -3.2 | -24.7 | 43.1 | 50.1 |
| Unconformity in North Polar Layered Deposits: ESP_018265_2595 ESP_018160_2595 (Interval in Earth days: 8) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 79.25 | 357. | 0.42 | -23.4 | 57.5 | 58.8 |
| North Polar Crater Change Detection: ESP_018471_2645 ESP_018498_2645 (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 | 84.32 | 120. | -0.4 | -16.8 | 62.0 | 63.1 |
| Channels in Tharsis Region: ESP_018349_2005 ESP_019338_2005 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.50 | 241. | 7.35 | -7.99 | 45.2 | 50.8 |
| Cracks and Fans on Dunes: ESP_018404_2610 ESP_018865_2610 (Interval in Earth days: 36) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 80.96 | 156. | 6.25 | 24.73 | 59.0 | 62.0 |
| North Polar Layered Deposits: ESP_018192_2680 ESP_019048_2680 (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 | 87.96 | 177. | -17. | -10.5 | 63.7 | 70.6 |
| Fresh 2-Kilometer Diameter Impact Crater: ESP_018219_2155 ESP_078576_2155 (Interval in Earth days: 4702) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 35.25 | 189. | -0.7 | 11.46 | 43.1 | 41.8 |
| Central Structure and Layering of a Large Impact Crater: ESP_018263_2230 ESP_018751_2230 (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 | 42.58 | 67.3 | -5.3 | -27.4 | 43.9 | 49.1 |
| Cones at Edge of North Polar Layered Deposits: ESP_018295_2580 ESP_026985_2580 (Interval in Earth days: 677) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 77.99 | 263. | -6.6 | -21.3 | 57.3 | 57.6 |
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