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.
| Inverted Crater atop Inverted Channel or Channel Belt: ESP_084095_1985 ESP_084530_1985 (Interval in Earth days: 33) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.26 | 358. | -13. | 5.923 | 58.0 | 51.3 |
| Light Layers at Base of Mounds in Oxia Colles: ESP_084096_2010 ESP_084320_2010 (Interval in Earth days: 17) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 20.63 | 330. | -8.3 | 22.19 | 59.3 | 54.8 |
| USGS Dune Database 3048-436: ESP_083794_1360 ESP_084005_1360 (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 | -43.6 | 304. | 1.72 | -13.4 | 41.8 | 41.4 |
| Interaction of Fluvial Ridge with Kilometer-Scale Polygonal Ridge System: ESP_083739_1990 ESP_084029_1990 (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 | 18.93 | 0.25 | -15. | -5.08 | 62.5 | 58.8 |
| Scarp Monitoring: ESP_083854_1295 ESP_075243_1295 (Interval in Earth days: 671) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -50.1 | 106. | 9.52 | -2.48 | 42.9 | 42.7 |
| Depression near Terminus of Lobate Deposit in Argyre Region: ESP_083780_1330 ESP_083846_1330 (Interval in Earth days: 5) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -46.7 | 327. | 4.09 | -15.7 | 42.6 | 43.6 |
| Hillslope Morphologies in Crater: ESP_083947_1515 ESP_084593_1515 (Interval in Earth days: 50) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -28.3 | 84.5 | 5.86 | -3.46 | 38.3 | 35.8 |
| South Polar Troughs: ESP_083993_0940 ESP_084045_0940 (Interval in Earth days: 4) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.1 | 308. | 5.53 | 20.25 | 64.6 | 63.6 |
| Stratigraphy Revealed by Hartwell Crater within Jezero Crater: ESP_084013_1985 ESP_083024_1985 (Interval in Earth days: 77) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | 18.44 | 77.7 | -10. | 24.56 | 58.9 | 63.0 |
| South Polar Carbon Dioxide Glacier Crevasses: ESP_083884_0930 ESP_075221_0930 (Interval in Earth days: 675) | Center lat. | Center long. | 1st half roll angle | 2nd half roll angle | 1st half incidence angle | 2nd half incidence angle | -86.9 | 20.2 | 24.9 | 12.53 | 63.3 | 64.8 |
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