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.
| Survey South Polar Layered Deposits: PSP_004593_0830 PSP_004984_0970 (Interval in Earth days: 30) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.6 | 140. | 0 | -19.2 | 72.0 | 65.8 |
| Seasonal Monitoring: PSP_005553_0980 PSP_005790_0980 (Interval in Earth days: 18) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.1 | 75.6 | -8.4 | 8.644 | 71.5 | 74.2 |
| Crater of Floor of Mawrth Vallis Channel: PSP_006755_2030 ESP_011383_2030 (Interval in Earth days: 361) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 22.95 | 341. | 20.9 | -3.88 | 37.8 | 60.1 |
| Central Peak Ring of Crater with Olivine and Diverse Bedrock Exposures: PSP_005816_1750 ESP_011512_1750 (Interval in Earth days: 444) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -4.95 | 64.9 | 0 | -25.3 | 33.6 | 59.6 |
| Channels or Flow Features with Inverted Topography on Arsia Mons: PSP_005915_1720 ESP_011690_1720 (Interval in Earth days: 450) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -7.81 | 242. | -5.1 | 8.736 | 33.9 | 56.6 |
| Breach of Crater Where Valley Begins: PSP_006229_1700 ESP_032245_1700 (Interval in Earth days: 2028) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -9.78 | 309. | 0 | 16.43 | 35.5 | 31.0 |
| Exposure of High-Latitude Polar Layered Deposits Not Well Observed: PSP_005157_0875 PSP_005577_0925 (Interval in Earth days: 32) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -87.2 | 152. | 0 | 14.21 | 71.5 | 75.0 |
| Oswego Region Unfrosted: PSP_005619_0945 PSP_005803_0945 (Interval in Earth days: 14) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -85.4 | 83.5 | 1.81 | 17.68 | 74.9 | 76.8 |
| Possible Pingo at the Border Between Fretted Crater Ejecta: PSP_006632_2240 PSP_010337_2240 (Interval in Earth days: 288) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 43.79 | 98.7 | 1.07 | -21.5 | 50.4 | 53.6 |
| Survey Central Peak Pit in Search of Exposed Layers: PSP_005649_1710 ESP_021551_1710 (Interval in Earth days: 1239) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -8.75 | 304. | -1.4 | 21.34 | 33.3 | 46.5 |
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