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.
Spider Evolution Unfrosted: PSP_004947_0930 PSP_005104_0930 (Interval in Earth days: 13) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.0 | 98.9 | -0.2 | 16.73 | 68.1 | 68.0 |
Crater Cut by Coprates Chasma: PSP_005148_1665 ESP_014114_1665 (Interval in Earth days: 699) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.7 | 303. | -4.6 | 22.21 | 34.6 | 32.5 |
Light-Toned Layered Rock Outcrop in Ladon Vallis: PSP_006637_1590 ESP_023383_1590 (Interval in Earth days: 1305) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -20.8 | 330. | 7.10 | 20.68 | 44.1 | 31.2 |
Layering in Graben Wall: PSP_005902_2265 ESP_085761_2265 (Interval in Earth days: 6222) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 45.97 | 229. | 3.76 | -10.1 | 60.9 | 56.0 |
Fresh Double-Layered Crater with Possible Ponded Materials: PSP_006945_2350 PSP_007235_2350 (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 | 54.57 | 190. | 1.13 | 12.28 | 54.1 | 50.5 |
Possible Exposures of Polar Layered Deposits in Area Not Well Observed: PSP_005014_0920 PSP_005276_0920 (Interval in Earth days: 20) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.8 | 93.8 | 5.80 | 17.37 | 69.5 | 70.9 |
Light-Toned Layered Rock Outcrop in Hellas Region: PSP_006700_1385 ESP_016141_1385 (Interval in Earth days: 736) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -41.1 | 53.1 | 5.27 | -12.5 | 58.1 | 68.9 |
Seasonal Monitoring: PSP_005455_0975 PSP_005547_0975 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.1 | 225. | 1.30 | 15.98 | 69.4 | 69.9 |
Basal Exposure of South Polar Layered Deposits: PSP_005102_1030 PSP_005155_1030 (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 | -76.8 | 132. | 7.05 | -13.4 | 60.2 | 62.0 |
Layered Bedrock Exposed in the Central Uplift of Martin Crater: PSP_005821_1585 ESP_011952_1585 (Interval in Earth days: 477) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 290. | -1.8 | 21.33 | 35.0 | 54.2 |
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