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.
A North Polar Crater: PSP_009689_2645 PSP_010084_2645 (Interval in Earth days: 31) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.33 | 120. | -1.7 | 12.07 | 62.3 | 65.3 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_009309_2725 PSP_009589_2675 (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 | 87.52 | 327. | -4.7 | -14.4 | 64.2 | 64.4 |
Basal Unit and North Polar Layered Deposits in Chasma Boreale Scarp: PSP_009995_2650 PSP_010128_2650 (Interval in Earth days: 10) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 85.06 | 0.70 | 19.4 | 5.177 | 65.3 | 66.6 |
Fresh Irregular Crater in Tyrrhena Terra : PSP_010113_1575 ESP_062503_1575 (Interval in Earth days: 4082) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -22.0 | 100. | -3.9 | 8.055 | 67.6 | 67.0 |
Survey Layering and Faulting in Layered Deposits in Candor Chasma: PSP_009328_1755 PSP_010172_1755 (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 | -4.38 | 288. | 5.36 | -21.3 | 57.5 | 59.5 |
Possible Pingos in Gusev Crater: PSP_009385_1655 PSP_009886_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 | -14.2 | 175. | -18. | 5.226 | 65.1 | 63.0 |
High-Latitude Exposure of North Polar Layered Deposits: PSP_009584_2675 PSP_009757_2675 (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 | 87.31 | 77.4 | -4.6 | -21.6 | 64.0 | 65.8 |
North Polar Terrain: PSP_009914_2750 PSP_010682_2650 (Interval in Earth days: 59) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 84.90 | 334. | 0 | 18.02 | 69.7 | 73.7 |
Slope Streaks on Nicholson Crater Mound: PSP_009371_1800 PSP_009516_1800 (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 | -0.00 | 195. | -5.9 | 9.471 | 55.9 | 55.0 |
Western Half of Heimdal Crater: PSP_009580_2485 PSP_009778_2485 (Interval in Earth days: 16) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 68.34 | 235. | 4.49 | -17.3 | 52.3 | 55.5 |
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