STS072-740-85
| NASA Photo ID | STS072-740-85 |
| Focal Length | 40mm |
| Date taken | 1996.01.18 |
| Time taken | 06:20:35 GMT |
Resolutions offered for this image:
640 x 480 pixels
640 x 480 pixels
Cloud masks available for this image:
MAP LOCATION
latitude/longitude of image
latitude/longitude of image
Spacecraft nadir point: 28.2° S, 91.7° E
Photo center point:
Photo center point:
Nadir to Photo Center:
Spacecraft Altitude: 166 nautical miles (307km)
IMAGE DETAILS
features and other details
features and other details
Country or Geographic Name: | INDIAN OCEAN |
Features: | PAN-CLOUDS |
Cloud Cover Percentage: | 55 (51-75)% |
Sun Elevation Angle: | 82° |
Sun Azimuth: | 331° |
CAMERA INFORMATION
information about camera used
information about camera used
Camera: | Hasselblad |
Focal Length: | 40mm |
Camera Tilt: | High Oblique |
Format: | 5046: Kodak, natural color positive, Lumiere 100/5046, ASA 100, standard base |
Film Exposure: | Normal |
| Additional Information | |
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| Width | Height | Annotated | Cropped | Purpose | Links |
|---|---|---|---|---|---|
| 640 pixels | 480 pixels | No | No | ISD 1 | Download Image |
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Image Caption: Closed Cellular Stratocumulus Cloud
Pattern in the Central Indian Ocean. This closed cell pattern is
usually associated with the anticyclonic flow of a high pressure
system. This type of cloud generally forms in shallow regions of cool,
moist maritime air moving over warmer water. This shallow region lies
under an inversion with descending warm dry air above which keep the
cloud heights from building. These closed cell clouds are getting
pulled along in a vertical wind shear.
Pattern in the Central Indian Ocean. This closed cell pattern is
usually associated with the anticyclonic flow of a high pressure
system. This type of cloud generally forms in shallow regions of cool,
moist maritime air moving over warmer water. This shallow region lies
under an inversion with descending warm dry air above which keep the
cloud heights from building. These closed cell clouds are getting
pulled along in a vertical wind shear.
