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.
Gullies in Dark Layers in Crater Wall: PSP_002212_1335 PSP_002291_1335 (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 | -46.2 | 184. | -6.7 | 21.92 | 73.0 | 70.0 |
Sample Main Channel of Athabasca Valles : PSP_002938_1890 PSP_003083_1890 (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 | 8.883 | 155. | 4.35 | 20.17 | 57.0 | 56.1 |
Potential Lobe of Lahar Flow Front: PSP_002042_2090 PSP_002108_2090 (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 | 28.85 | 134. | 5.87 | -13.1 | 53.3 | 55.7 |
North Polar Trough with Curved Exposure: PSP_001738_2670 PSP_001871_2670 (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 | 87.09 | 92.7 | -1.8 | -13.5 | 74.0 | 76.3 |
Terraced Fan in Memnonia: PSP_001644_1715 PSP_001842_1715 (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 | -8.60 | 200. | 21.0 | -7.60 | 56.5 | 58.2 |
Layered Deposits within an Unnamed Crater in Arabia Terra: PSP_002100_1840 ESP_060054_1840 (Interval in Earth days: 4515) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 4.165 | 354. | 0 | -10.2 | 54.3 | 38.9 |
Sublimation Processes and Spider Evolution : PSP_002652_0930 PSP_002651_0930 (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 | -86.9 | 96.5 | 7.08 | 22.50 | 87.8 | 86.4 |
Gamboa Crater Central Uplift in Acidalia Planitia : PSP_002721_2210 ESP_028724_2210 (Interval in Earth days: 2026) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 40.77 | 315. | 0.64 | -12.1 | 66.1 | 59.9 |
Light-Toned Layered Bedrock Exposed in Valles Marineris : PSP_002722_1665 PSP_003355_1665 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -13.1 | 295. | 2.08 | -13.4 | 56.0 | 53.6 |
Interior Channel in Parana Valles: PSP_002008_1560 PSP_002285_1560 (Interval in Earth days: 22) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -23.9 | 350. | -0.6 | -27.3 | 63.5 | 63.7 |
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