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.
Scarp: ESP_019047_2640 ESP_019298_2640 (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 | 83.88 | 235. | 0.05 | -12.8 | 67.1 | 71.2 |
Linear Dunes and Sand Sheets in Herschel Crater: ESP_016916_1655 ESP_017417_1655 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -14.1 | 129. | 5.50 | 22.91 | 58.0 | 60.0 |
Layered Bedrock near Oyama Crater: ESP_018820_2035 ESP_019664_2035 (Interval in Earth days: 66) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 23.40 | 341. | 16.2 | -9.56 | 45.5 | 53.5 |
Glacier?: ESP_018857_2225 ESP_019358_2225 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 42.21 | 50.5 | -6.4 | 8.421 | 47.8 | 51.8 |
Alluvial Fan in Far Western Terra Tyrrhena: ESP_018738_1585 ESP_019160_1585 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 67.0 | 0.22 | -17.5 | 66.6 | 65.9 |
Central Pit of an Impact Crater: ESP_018703_1570 ESP_019204_1570 (Interval in Earth days: 39) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -22.6 | 303. | -7.7 | 11.51 | 67.9 | 64.3 |
Light-Toned Layered Rock in Ridge in Coprates Chasma: ESP_018545_1670 ESP_019824_1670 (Interval in Earth days: 100) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 294. | 1.64 | 20.31 | 61.7 | 56.2 |
North Polar Residual Cap: ESP_018621_2620 ESP_018872_2620 (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 | 81.78 | 355. | -1.4 | -19.1 | 61.6 | 65.2 |
Crater Ejecta Lower Than Plains: ESP_018709_2290 ESP_019197_2290 (Interval in Earth days: 38) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 48.73 | 127. | 13.4 | -11.4 | 46.3 | 53.4 |
Lava Channel on the North Flank of Ascraeus Mons: ESP_018520_1920 ESP_018665_1920 (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 | 11.95 | 254. | -4.6 | 13.12 | 49.3 | 48.3 |
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