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.
Region Shows Differentially-Eroded Fan Deposits: PSP_005829_1580 PSP_006686_1580 (Interval in Earth days: 67) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -21.8 | 72.8 | -8.0 | 3.642 | 35.7 | 45.6 |
Fresh Double-Layered Crater with Possible Ponded Materials: PSP_006945_2350 PSP_007235_2350 (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 | 54.57 | 190. | 1.13 | 12.28 | 54.1 | 50.5 |
Diverse Stratigraphic Layers Exposed in Depression: PSP_006290_1590 PSP_010575_1590 (Interval in Earth days: 334) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -20.8 | 85.3 | 0 | 16.21 | 39.8 | 63.6 |
Possible Fissure Source For Floodwaters: PSP_006788_1955 PSP_010361_1955 (Interval in Earth days: 278) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 15.30 | 163. | 2.45 | 16.72 | 37.6 | 50.3 |
Seasonal Monitoring: PSP_005455_0975 PSP_005547_0975 (Interval in Earth days: 7) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -82.1 | 225. | 1.30 | 15.98 | 69.4 | 69.9 |
Gullies: PSP_006821_1270 ESP_024121_1270 (Interval in Earth days: 1349) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -52.6 | 351. | -0.1 | -25.5 | 68.9 | 63.9 |
Basal Exposure of South Polar Layered Deposits: PSP_005049_1075 PSP_005247_1075 (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 | -72.1 | 138. | 1.11 | -21.4 | 56.4 | 59.9 |
Delta-Like Deposit on Crater Floor: PSP_005699_1425 ESP_012041_1425 (Interval in Earth days: 494) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -37.0 | 22.7 | 6.50 | 20.92 | 39.8 | 55.2 |
Possible Collapse Feature in Impact Crater Ejecta: PSP_005933_2200 ESP_011286_2200 (Interval in Earth days: 417) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 39.71 | 105. | -6.4 | 11.69 | 56.3 | 62.4 |
Northwest Hellas Region Landforms: PSP_006845_1390 ESP_015943_1390 (Interval in Earth days: 709) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -40.5 | 54.2 | 2.86 | 28.43 | 60.2 | 63.1 |
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