ISS012-E-14621
| NASA Photo ID | ISS012-E-14621 |
| Focal Length | 400mm |
| Date taken | 2006.01.06 |
| Time taken | 08:40:28 GMT |
Cloud masks available for this image:
Spacecraft nadir point: 29.3° N, 89.8° E
Photo center point: 28.6° N, 90.5° E
Photo center point by machine learning:
Photo center point: 28.6° N, 90.5° E
Photo center point by machine learning:
Nadir to Photo Center: Southeast
Spacecraft Altitude: 185 nautical miles (343km)
Country or Geographic Name: | CHINA |
Features: | PUMA LAKE, ICE, TIBETAN PLATEAU |
| Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 10 (1-10)% |
Sun Elevation Angle: | 26° |
Sun Azimuth: | 220° |
Camera: | Kodak DCS760c Electronic Still Camera |
Focal Length: | 400mm |
Camera Tilt: | 18 degrees |
Format: | 3060E: 3060 x 2036 pixel CCD, RGBG array |
Film Exposure: | |
| Additional Information | |
| Width | Height | Annotated | Cropped | Purpose | Links |
|---|---|---|---|---|---|
| 1520 pixels | 1008 pixels | No | No | Not enhanced | Download Image |
| 639 pixels | 435 pixels | No | No | Download Image |
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Image Caption: ISS012-E-14621 (6 Jan. 2006) --- A portion of Lake Puma Yumco and parts of Tibet and China are featured in this image photographed by an Expedition 12 crew member on the International Space Station. The alpine lakes of the Tibetan Plateau are some of the most remote in the world. This image depicts Lake Puma Yumco during the winter season. The lake is located at an elevation of 5,030 meters above sea level, and is considered ultraoligotrophic in that nutrient concentrations in both the water column and lake sediments are extremely low. Water in such lakes tends to be blue to blue-green and have high clarity due to the lack of abundant photosynthesizing organisms such as phytoplankton. Water color change in these lakes is usually due to shallowing of the water - blue indicating deeper water. The maximum dimensions of the lake are 31 kilometers by 14 kilometers, indicating that the ice blocks range from less than ten to hundreds of meters in diameter. According to scientists, the ice pattern is caused by repeated cycles of freezing, fracturing, and refreezing of the ice due to variations in temperature and wind-induced ice motion. A prominent white linear feature across the center of the lake (not visible in this image) is suggestive of an ice ridge formed by east-west winds subsequently highlighted by snow.
