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.
Changes in Intracrater Dunes: ESP_023130_1345 ESP_023420_1345 (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 | -45.0 | 42.0 | 3.77 | 28.52 | 41.4 | 43.5 |
Small Mounds in Chryse Planitia: ESP_023159_1995 ESP_023225_1995 (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 | 19.36 | 322. | -2.4 | -20.9 | 45.9 | 46.3 |
Putative Ice-Free Geyser Locale: ESP_023103_0945 ESP_023076_0945 (Interval in Earth days: 2) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.4 | 103. | -6.6 | 8.719 | 73.2 | 71.6 |
Gully Change Detection: ESP_023111_1330 ESP_023032_1330 (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 | -46.3 | 197. | 29.0 | 2.043 | 40.3 | 41.2 |
Lobate Flow on Side of Mound: ESP_023365_1445 ESP_023655_1445 (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 | -35.1 | 104. | 6.28 | 26.96 | 38.1 | 40.6 |
Well-Preserved 8-Kilometer Diameter Crater Near Tharsis Tholus: ESP_023372_1960 ESP_023662_1960 (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 | 15.81 | 267. | 1.18 | 24.59 | 40.9 | 36.6 |
Intracrater Dunes: ESP_023271_1120 ESP_023284_1120 (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 | -67.8 | 163. | -21. | 3.119 | 61.4 | 60.2 |
Gullies in Crater Wall: ESP_023494_1410 ESP_023995_1410 (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 | -38.6 | 183. | 0.3 | 19.56 | 42.1 | 48.8 |
South Polar Layered Deposits: ESP_023430_0925 ESP_023521_0925 (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 | -87.6 | 192. | 8.06 | 21.01 | 79.6 | 79.7 |
Gullies in Resistant Layers of Crater Wall: ESP_023289_1335 ESP_022999_1335 (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 | -46.1 | 18.9 | 26.3 | -0.21 | 42.6 | 41.0 |
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