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.
Good-Looking Gullies: PSP_004777_1090 PSP_004843_1090 (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 | -70.6 | 2.11 | 5.76 | -2.69 | 53.2 | 54.0 |
Alluvial Fans in Unnamed Crater: PSP_006528_1585 PSP_007095_1585 (Interval in Earth days: 44) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 67.1 | 0 | -14.3 | 43.3 | 52.6 |
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 |
Gullies Within Central Pit of Bamberg Crater: PSP_006794_2200 PSP_010301_2200 (Interval in Earth days: 274) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.66 | 356. | -3.9 | 21.59 | 46.9 | 48.7 |
Layered Sediments in Tithonium Chasma: PSP_005281_1750 PSP_005703_1750 (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 | -4.92 | 270. | 10.9 | -5.09 | 35.2 | 34.1 |
Gullies in Southern Latitude Crater: PSP_005701_1445 PSP_005991_1445 (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 | -35.2 | 328. | 0.44 | 26.02 | 39.2 | 41.2 |
36 Gullies Previously Identified and Fully Described in MOC Image M03-03547: PSP_005646_1360 ESP_022682_1360 (Interval in Earth days: 1327) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -43.7 | 34.1 | -24. | -7.08 | 45.0 | 38.1 |
Floor of Ares Vallis: PSP_006940_1900 PSP_007876_1900 (Interval in Earth days: 73) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 10.11 | 334. | -1.8 | 20.02 | 38.4 | 42.9 |
Mounds in Arcadia Region: PSP_006852_2200 PSP_007142_2200 (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 | 39.53 | 213. | -6.8 | 10.53 | 46.6 | 43.4 |
Possible Exposures of Polar Layered Deposits in Area Not Well Observed: PSP_005014_0920 PSP_005276_0920 (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 | -87.8 | 93.8 | 5.80 | 17.37 | 69.5 | 70.9 |
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