Sunglint in Astronaut Photography of Earth
Earth Sciences and Image Analysis Laboratory, Johnson Space Center
May 21, 2003

This mosaic of two photographs shows the brighter center portion of the sunglint pattern (lower right) and how that pattern is reduced as you mover further from the glitter point. In this view of the Red Sea, the major source of reflection is a thin layer of oily film that is produced by both shipping traffic and the natural biological activity of marine life. Photographs ISS006-E-45935 and ISS006-E-45936, Kodak digital camera with 180-mm lens; Shuttle altitude = 209 n. mi. (387 km.).

Sunlight illuminates a water body, such as a lake, stream, or, ocean, a portion of the light will penetrate the water body while the remainder will be reflected into the atmosphere from the water surface. When viewed from an airplane or from space, the light reflected from the water surface, referred to as "sunglint," will appear as a circular bright area on the water surface in the direction of the Sun. The location and size of the sunglint is a function of the location of the Sun in the sky, the location of the observer, and the roughness of the water surface. If the water surface were perfectly flat, the surface would appear as an image of the solar disk. However, the surface of a natural waterbody is rarely flat. Wind blowing across the water surface produces waves, small waves at first then gradually larger as the wind increases speed and is sustained. The presence of waves tends to disperse the surface-reflected light, and the result is a spreading of the sunglint pattern.


A portion of the sunlight illuminating a water surface is reflected into the atmosphere. From a smooth water surface(a), light is reflected at a narrow solid angle; from a rough water surface(b), reflected light will be dispersed over a larger solid angle.

Photographs from space of the ocean sunglint pattern are a valuable tool for studying physical oceanographic and atmospheric processes and other phenomena that affect surface roughness. Variability in windspeed and direction, surface water currents, and water temperature all produce unique signatures within the sunglint pattern. A good example is a man-made oil slick that results from bilge pumping. Viewed form a ship, the slick will appear as a long narrow area of smooth water-the oil tends to damp out small capillary waves. Viewed within the sunglint pattern, the slick will appear very bright near the center of the pattern. Because this area is more mirror-like than the surrounding water, more sunlight will be reflected towards the observer.

However, near the periphery of the pattern, the slick will appear darker than the surrounding water, as the sunlight reflected from the smooth water is directed away from the observer.

STS038-83-38
Oil slicks tend to dampen surface capillary waves, making the water smoother than the surrounding oil-free water. As a result, slicks appear brighter in the center portion of the sunglint pattern (A) and darker on the periphery (B). In this view of the Arabian Sea, bilge pumping has produced an oil slick along the coast of South Yemen (15.5° N, 52.5° E). Photograph STS038-83-38; Hasselblad camera with 250-mm lens and color visible film; Shuttle altitude = 120 n. mi. (222 km.).

Often the center of the sunglint is so bright that the film becomes overexposed and the fine detail within the pattern is washed out. It is therefore best to view the outer portions of the pattern.

Water features in the sunglint pattern appear to the astronaut to be extremely transient, visible only briefly (one to several seconds) as the spacecraft passes rapidly overhead. Often features found in photographs of the sunglint pattern are noticed only after the images are analyzed on Earth.

Sunglint can also greatly aid in distinguishing drainage patterns on land. While dry land will absorb and scatter the sunlight in a variety of directions, any water (e.g., lakes, rivers, streams, creeks) will reflect much more light in the direction of the observer. The result is high contrast between the water areas (appearing bright) and the dry land (appearing dark)


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