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.
Crater of Floor of Mawrth Vallis Channel: PSP_006755_2030 ESP_011383_2030 (Interval in Earth days: 361) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.95 | 341. | 20.9 | -3.88 | 37.8 | 60.1 |
Sulfates in Ius Chasma: PSP_006652_1725 ESP_023398_1725 (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 | -7.47 | 279. | 0 | 14.79 | 39.1 | 30.7 |
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 |
Gullies Cut into Light-Toned Rock: PSP_006888_1410 ESP_016184_1410 (Interval in Earth days: 724) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -38.4 | 319. | 2.83 | -23.2 | 59.4 | 68.2 |
Thermally-Distinct Rays Emanating from Gratteri Crater: PSP_006510_1635 ESP_020922_1635 (Interval in Earth days: 1123) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -16.3 | 197. | 0 | 27.48 | 40.6 | 49.7 |
Seasonal Monitoring: PSP_005750_0965 PSP_005921_0965 (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 | -83.6 | 99.6 | -2.1 | 13.97 | 75.7 | 77.5 |
Channels or Flow Features with Inverted Topography on Arsia Mons: PSP_005915_1720 ESP_011690_1720 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.81 | 242. | -5.1 | 8.736 | 33.9 | 56.6 |
Central Peak with Layered Bedrock: PSP_005683_1640 ESP_011458_1640 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -15.7 | 96.8 | 5.59 | 18.89 | 32.6 | 57.3 |
Oswego Region Unfrosted: PSP_005619_0945 PSP_005803_0945 (Interval in Earth days: 14) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.4 | 83.5 | 1.81 | 17.68 | 74.9 | 76.8 |
Light-Toned Layers in Noctis Labyrithus: PSP_006890_1695 ESP_015975_1695 (Interval in Earth days: 708) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -10.4 | 261. | 2.52 | -22.8 | 42.9 | 48.0 |
Page 796 of 851 (8,502 images) |