Stereo Pairs 
An explanation of stereo pairs and their use (PDF)  

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.

Exposed Layers in Olympia Mensae Icy Outliers:   ESP_089774_2545   ESP_089787_2545   (Interval in Earth days: 1)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
74.13

95.1

-4.3

10.35

64.8

63.9

Streamlined Shape and Possible Bar South of Semeykin Crater:   ESP_089883_2195   ESP_090028_2195   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.01

8.16

-0.2

14.06

53.3

53.8

Crater in Arabia Terra:   ESP_089804_2205   ESP_090160_2205   (Interval in Earth days: 28)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.96

7.23

-21.

-7.62

54.5

57.6

Survey of Terrain around Ice-Exposing Crater:   ESP_089639_2195   ESP_089507_2195   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
39.10

190.

-9.9

20.77

51.6

47.5

Hillslope Morphologies in Roddy Crater:   ESP_089885_1585   ESP_090030_1585   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-21.1

320.

5.83

24.57

64.9

62.7

Scarp Contact:   ESP_089889_1920   ESP_090166_1920   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
11.85

207.

1.64

-17.1

53.2

56.1

Large Alluvial Fan in Kasei Valles:   ESP_089846_2065   ESP_089991_2065   (Interval in Earth days: 11)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
26.23

300.

-2.1

14.95

51.9

51.7

Valley Attached to Northern Mid-Latitude Crater:   ESP_089316_2135   ESP_089461_2135   (Interval in Earth days: 12)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
33.34

7.71

5.13

17.17

47.2

47.2

Potential Compound Dune:   ESP_089362_2590   ESP_089415_2590   (Interval in Earth days: 4)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
78.72

174.

6.27

-7.76

61.5

63.0

Dune Interaction with Residual Polar Ice:   ESP_089286_2595   ESP_089405_2595   (Interval in Earth days: 9)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
79.46

89.3

3.05

-13.8

61.3

63.6


  


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