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.
Exposure of High-Latitude Polar Layered Deposits Not Well Observed: PSP_005971_0890 PSP_005957_0910 (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 | -88.7 | 251. | 18.6 | 19.51 | 83.1 | 82.5 |
Gullies with Extensive Debris Aprons: PSP_006960_1465 ESP_076916_1465 (Interval in Earth days: 5451) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -33.1 | 152. | 5.24 | 24.98 | 56.8 | 47.6 |
Pitted Layers Northeast of Hellas Region: PSP_006198_1525 ESP_032702_1525 (Interval in Earth days: 2065) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -27.3 | 78.0 | 0 | -26.6 | 41.6 | 43.7 |
Sinuous Features in Light-Toned Material: PSP_006583_1775 PSP_010789_1775 (Interval in Earth days: 328) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -2.28 | 3.05 | 0 | -17.1 | 37.2 | 58.5 |
Deeply-Penetrating Structure within Polar Layered Deposits: PSP_005076_0940 PSP_005207_0940 (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 | -86.1 | 172. | -8.4 | 5.833 | 69.3 | 69.2 |
Lobate Margin of Impact Ejecta: PSP_006835_2085 PSP_007481_2085 (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 | 28.13 | 319. | -5.9 | 4.424 | 41.5 | 40.0 |
Eastern Side of Hale Crater Ridge with Gullies on Both Sides: PSP_005833_1445 ESP_011753_1445 (Interval in Earth days: 462) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -35.1 | 324. | 0.11 | 25.34 | 40.8 | 58.2 |
Layers in Memnonia Sulci: PSP_006616_1730 ESP_024285_1730 (Interval in Earth days: 1377) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -6.70 | 182. | -4.8 | 22.96 | 38.8 | 35.4 |
Gorgonum Chaos: PSP_006906_1425 ESP_016004_1425 (Interval in Earth days: 709) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.2 | 188. | 1.20 | 29.59 | 58.9 | 61.5 |
Polar Layered Deposit Stratigraphy Near Chasma Australe: PSP_004840_0940 PSP_005078_0940 (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 | -86.1 | 94.2 | 20.6 | 6.758 | 64.4 | 67.7 |
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