| Ocean Dynamics, Sea of Crete-Sea of Karpathos-November
1985: Despite the underexposure of this northeast-looking
photograph of the Sea of Crete and the small amount of information that
can be gleaned from the islands (dark areas silhouetted against the water
background), a camera-Sun relationship produced a phenomenon called sunglint.
Sunglint is produced when a camera focuses on a water surface where light
from the water surface reflects through the camera lens onto the film.
Geometrically, this effect occurs only when the view focuses toward the
Sun. The result of this interaction produces an image that can be used
to analyze dynamic ocean features. Sea surface roughness determines the
intensity or amount of reflected energy that is portrayed on the film—a
smooth sea surface is more highly reflective than a rough sea, thereby
producing areas on the film that are brighter. This sunglint photograph
shows a tremendous amount of dynamic surface water detail—spiral eddies
in the Sea of Crete north of the island of Crete, two very pronounced V-shaped
ship wakes in the darker water off the northeast coast of Crete (indicative
of ships traveling at high speeds through a rather calm sea), and island
wakes around the smaller islands north of Crete. SOURCE:
NASA |