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.

Changes in Intracrater Dunes:   ESP_023130_1345   ESP_023420_1345   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-45.0

42.0

3.77

28.52

41.4

43.5

Small Mounds in Chryse Planitia:   ESP_023159_1995   ESP_023225_1995   (Interval in Earth days: 5)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
19.36

322.

-2.4

-20.9

45.9

46.3

Putative Ice-Free Geyser Locale:   ESP_023103_0945   ESP_023076_0945   (Interval in Earth days: 2)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-85.4

103.

-6.6

8.719

73.2

71.6

Gully Change Detection:   ESP_023111_1330   ESP_023032_1330   (Interval in Earth days: 6)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-46.3

197.

29.0

2.043

40.3

41.2

Lobate Flow on Side of Mound:   ESP_023365_1445   ESP_023655_1445   (Interval in Earth days: 22)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-35.1

104.

6.28

26.96

38.1

40.6

Well-Preserved 8-Kilometer Diameter Crater Near Tharsis Tholus:   ESP_023372_1960   ESP_023662_1960   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
15.81

267.

1.18

24.59

40.9

36.6

Intracrater Dunes:   ESP_023271_1120   ESP_023284_1120   (Interval in Earth days: 1)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-67.8

163.

-21.

3.119

61.4

60.2

Gullies in Crater Wall:   ESP_023494_1410   ESP_023995_1410   (Interval in Earth days: 39)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-38.6

183.

0.3

19.56

42.1

48.8

South Polar Layered Deposits:   ESP_023430_0925   ESP_023521_0925   (Interval in Earth days: 7)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-87.6

192.

8.06

21.01

79.6

79.7

Gullies in Resistant Layers of Crater Wall:   ESP_023289_1335   ESP_022999_1335   (Interval in Earth days: 23)
Center lat.Center long.1st half roll angle2nd half roll angle1st half incidence angle2nd half incidence angle
-46.1

18.9

26.3

-0.21

42.6

41.0


  


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