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.
Landforms in Athabasca Valles: PSP_006696_1895 PSP_007408_1895 (Interval in Earth days: 55) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 9.346 | 155. | 3.28 | -6.76 | 36.8 | 42.0 |
Evolution of Surface Near the Granicus and Tinjar Valles: PSP_005932_2080 ESP_057873_2080 (Interval in Earth days: 4047) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 27.73 | 135. | -18. | 2.277 | 48.7 | 58.1 |
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 | 72.1 | 65.8 |
Spider Evolution Unfrosted: PSP_004947_0930 PSP_005104_0930 (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 | -87.0 | 98.9 | -0.2 | 16.73 | 68.1 | 68.0 |
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 |
Spallanzani Crater - Swirl Patterns in Lower Layers along Northern Margin: PSP_005565_1220 PSP_005842_1220 (Interval in Earth days: 21) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -57.7 | 86.3 | -5.0 | -20.8 | 52.1 | 57.2 |
Lineated Valley Flow and Dissected Mantle Terrain in Chaotic Region: PSP_006807_2185 PSP_007097_2185 (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 | 38.22 | 2.06 | -3.1 | 14.00 | 46.0 | 42.9 |
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 |
Crater in Tyrrhena Terra: PSP_006830_1745 ESP_069692_1740 (Interval in Earth days: 4898) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -5.58 | 99.6 | -3.9 | -21.0 | 40.7 | 61.4 |
Layered Bedrock Exposed in the Central Uplift of Martin Crater: PSP_005821_1585 ESP_011952_1585 (Interval in Earth days: 477) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.4 | 290. | -1.8 | 21.33 | 35.0 | 54.2 |
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