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.
| Flow Ridge in Nereidum Montes: ESP_085587_1340 ESP_085732_1340 (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 | -45.6 | 310. | -6.8 | 16.93 | 55.1 | 56.2 |
| Glacier-Like Form Terminus into Valley Fill: ESP_085405_2185 ESP_085748_2185 (Interval in Earth days: 26) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 37.97 | 226. | -4.2 | -17.4 | 54.5 | 51.5 |
| Alluvial Fans in Kasei Valles: ESP_085574_2030 ESP_085640_2030 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.67 | 293. | 15.8 | 1.691 | 42.0 | 42.6 |
| Inverted Channel in Noachis Terra: ESP_085453_1585 ESP_085519_1585 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.1 | 2.69 | 9.81 | -7.34 | 38.4 | 40.4 |
| Ridge-Crater Relationships in Osuga Valles: ESP_085349_1650 ESP_085982_1650 (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 | -14.7 | 321. | -4.2 | 3.855 | 36.6 | 42.7 |
| Small Pedestal Crater: ESP_085103_2135 ESP_085169_2135 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 33.31 | 189. | 9.68 | -7.03 | 54.3 | 54.3 |
| Dunes in Terra Cimmeria: ESP_084986_1415 ESP_085342_1415 (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 | -38.2 | 154. | -1.9 | 14.25 | 41.6 | 45.1 |
| South Polar Layered Deposits Survey: ESP_085034_0920 ESP_067441_0920 (Interval in Earth days: 1371) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.7 | 323. | 17.1 | 28.9 | 77.1 | 76.9 |
| Hillslope Shapes on Holden Crater Rim: ESP_085006_1550 ESP_085151_1550 (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 | -24.7 | 325. | 2.17 | 18.92 | 36.0 | 35.9 |
| Raised Glacier-Like Forms in Arabia Terra: ESP_085043_2150 ESP_085109_2150 (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 | 34.67 | 27.6 | 6.88 | -10.0 | 56.2 | 56.3 |
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