STS042-72-16
NASA Photo ID | STS042-72-16 |
Focal Length | 100mm |
Date taken | 1992.01.23 |
Time taken | 03:15:47 GMT |
Cloud masks available for this image:
Country or Geographic Name: | RUSSIAN FEDERATION |
Features: | ICE PATTERNS-G. OZERNOY |
Features Found Using Machine Learning: | |
Cloud Cover Percentage: | 5 (1-10)% |
Sun Elevation Angle: | 9° |
Sun Azimuth: | 209° |
Camera: | Hasselblad |
Focal Length: | 100mm |
Camera Tilt: | 51 degrees |
Format: | 5017: Kodak, natural color positive, Ektachrome, X Professional, ASA 64, standard base |
Film Exposure: | Normal |
Additional Information | |
Width | Height | Annotated | Cropped | Purpose | Links |
---|---|---|---|---|---|
5700 pixels | 6000 pixels | No | No | Download Image | |
500 pixels | 526 pixels | No | No | Download Image | |
640 pixels | 480 pixels | No | No | Download Image |
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Image Caption:
STS042-71-080 & STS042-72-016 Ice Flow Patterns off the Eastern
Coast of Kamchatka Both of these slides show ice flow
patterns in the Gulf of Ozernoy on the east coast of Kamchatka
(57.0! N, 163.3! E). The time difference between slides is only
10 seconds, but they provide different perspectives on the Gulf.
Little is known of near- coastal current flow in this area,
although the general flow offshore is southward. Thin sea-ice
patterns near the shore indicate offshore winds blowing in a
southeasterly direction. The cyclonic ice pattern at the outer
edge of the Gulf may be more induced by coastal currents than by
wind.
STS042-71-080 & STS042-72-016 Ice Flow Patterns off the Eastern
Coast of Kamchatka Both of these slides show ice flow
patterns in the Gulf of Ozernoy on the east coast of Kamchatka
(57.0! N, 163.3! E). The time difference between slides is only
10 seconds, but they provide different perspectives on the Gulf.
Little is known of near- coastal current flow in this area,
although the general flow offshore is southward. Thin sea-ice
patterns near the shore indicate offshore winds blowing in a
southeasterly direction. The cyclonic ice pattern at the outer
edge of the Gulf may be more induced by coastal currents than by
wind.