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(NASA Crew Earth Observations)

Photographing the Earth from the International Space Station

Astronaut Photography of Earth - Display Record


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File NameFile Size (bytes)WidthHeightAnnotatedCroppedPurposeComments
View ISS030-E-234965.JPG 67812640425 No No
View ISS030-E-234965.JPG 267174540497 Yes Yes NASA's Earth Observatory web site
View ISS030-E-234965.JPG 7078841000921 No Yes NASA's Earth Observatory web site
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Mission: ISS030 Roll: E Frame: 234965 Mission ID on the Film or image: ISS030
Country or Geographic Name: NAMIBIA
Center Point: Latitude: -18.5 Longitude: 16.0 (Negative numbers indicate south for latitude and west for longitude)

Stereo: (Yes indicates there is an adjacent picture of the same area)


Camera Tilt: 25
Camera Focal Length: 180mm
Camera: N2: Nikon D2Xs
Film: 4288E : 4288 x 2848 pixel CMOS sensor, RGBG imager color filter.


Film Exposure:
Percentage of Cloud Cover: 10 (0-10)


GMT Date: 20111230 (YYYYMMDD) GMT Time: 082641 (HHMMSS)
Nadir Point Latitude: -17.1, Longitude: 15.0 (Negative numbers indicate south for latitude and west for longitude)

Nadir to Photo Center Direction: Southeast
Sun Azimuth: 106 (Clockwise angle in degrees from north to the sun measured at the nadir point)
Spacecraft Altitude: 216 nautical miles (400 km)
Sun Elevation Angle: 53 (Angle in degrees between the horizon and the sun, measured at the nadir point)
Orbit Number:


Note: This caption refers to the image versions labeled "NASA's Earth Observatory web site".

This astronaut photograph shows the white, salt-covered floor of the northwest corner of the great dry lake in northern Namibia known as the Etosha Pan (lower image margin). Two rivers, the Ekuma and Oshigambo, transport water from the north down to the Etosha Pan proper. In a relatively rare event, water from recent rains has flowed down the larger Ekuma River—in which it appears as a thin blue line within the generally light grey-green floodplain—and fills a lobe of the lake with light green water (lower right quarter of image). Water has also flowed into a small offshoot dry lake where it appears a brighter green (upper left quarter of image).

Other smaller lakes at image top center and image left show red and brown water colors. The different colors of lake water are determined by the interplay of water depth and resident organisms such as algae; the algae color varies depending on water temperature and salinity. A similar process is observed in pink and red floodwaters ponded in Lake Eyre, a usually dry lake in Australia’s arid center. In this case it is known that the coloration is indeed due to algae growth.

Typically, little river water or sediment reaches the floor of the Etosha dry lake because water seeps into the riverbeds along their courses. The floor of the pan itself is seldom seen with even a thin sheet of water. In this image, there was enough surface flow to reach the pan, but too little to flow beyond the inlet bay. A prior flood event, when water entered the pan via the Oshigambo River, was documented in astronaut imagery in 2006.

The straight line that crosses the image from upper left to upper right is the northern fence line of Namibia’s Etosha National Park. This straight, 3 meter-high fence keeps wildlife from crossing into the numerous small farms of the relatively densely populated Owambo region of Namibia, north of the pan. The large Etosha dry lakebed (120 km or 75 mi long) is the center of Namibia’s largest wildlife park, a major tourist attraction.

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