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.
| Exposure of Polar Layered Deposits in Area Not Well Observed: PSP_009359_2715 PSP_009400_2685 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.42 | 42.9 | -12. | -12.2 | 64.8 | 64.2 |
| Seasonal Monitoring of Polar Crater with Summer Ice: PSP_009364_2505 ESP_018766_2505 (Interval in Earth days: 732) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 70.05 | 13.8 | -2.3 | -22.2 | 52.5 | 58.1 |
| Central Peak and Pit with Bedrock Exposures: PSP_010389_1670 ESP_025751_1670 (Interval in Earth days: 1197) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -12.9 | 123. | 4.69 | -15.0 | 61.2 | 57.5 |
| Mound in Small Crater in Utopia Region: PSP_010324_2195 PSP_010390_2195 (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 | 39.39 | 91.8 | -2.9 | -18.2 | 51.0 | 53.1 |
| High-Latitude Exposure of North Polar Layered Deposits: PSP_009352_2680 PSP_009618_2680 (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 | 87.98 | 258. | -6.4 | -18.5 | 63.9 | 65.0 |
| Chain of Vents on Arsia Mons Caldera Floor: PSP_009343_1700 PSP_009976_1700 (Interval in Earth days: 49) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.69 | 239. | 16.3 | -7.18 | 60.1 | 61.2 |
| Eroding Margin of Low Latitude North Polar Layered Deposits: PSP_009938_2640 PSP_010176_2640 (Interval in Earth days: 19) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 83.87 | 139. | 19.6 | 5.57 | 63.3 | 66.3 |
| Alcove with Bright Rocky Slope Streaks: PSP_009762_1905 PSP_009907_1905 (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 | 10.40 | 318. | -0.3 | 15.26 | 51.2 | 50.3 |
| Interaction of Cratered Cone and Crater Ejecta: PSP_009906_2225 PSP_010196_2225 (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 | 42.33 | 343. | -7.7 | 14.62 | 48.0 | 48.7 |
| Exposure of Polar Layered Deposits: PSP_010116_2680 PSP_010075_2720 (Interval in Earth days: 3) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 88.20 | 303. | -10. | -10.3 | 69.5 | 69.6 |
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