The Science of Sunglint

Sunglint Crete Annotated

July 3, 2014

If you look frequently at satellite imagery or astronaut photography, you have probably noticed bright patches of light that can make certain bodies of water gleam with unusual color. (If not, look at these examples in the waters around Cape Cod and the Lesser Antilles, as well as rivers in Brazil.) That gleam is caused by sunglint, an optical phenomenon that occurs when sunlight reflects off the surface of water at the same angle that a satellite sensor views it. The result is a mirror-like specular reflection of sunlight off the water and back at the satellite sensor or astronaut.

Sunglint

The mirror-like reflection of the Sun off a water surface in a satellite image. If the ocean were as smooth as a mirror, a sequence of nearly perfect reflections of the Sun would appear in a line along the track of the satellite’s orbit. Because the ocean is never perfectly smooth or calm, however, the Sun’s reflection gets blurred as the light is scattered in all directions by waves. The blurred reflection gives the ocean surface a washed out appearance—the sunglint region.

If bodies of water were perfectly smooth, a sequence of nearly perfect reflections of the Sun would appear in a line along the track of the satellite’s orbit. In reality, water surfaces are irregular and often in motion due to waves and currents, so the sunlight gets scattered in many directions and leaves blurry streaks of light in the swaths of satellite data. For instance, notice the strips of sunglint in the mosaic below. All of the data was collected by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite on July 3, 2014.

The combination of sunglint, wind patterns, and island shapes around Crete and the Aegean islands made for a particularly spectacular scene that day. (See the image at the top of this page.) Although sunglint washes out many features, it also reveals details about the water and atmospheric circulation that are usually hidden. In this case, sunglint exposed wakes caused by north and northwest winds that roughened and smoothed the water surface behind Crete and the other islands.

The islands create a sort of wind shadow—blocking, slowing, and redirecting air flow. That wind, or lack of it, piles up waves and choppy water in some places and calms the water surface in others, changing how light is reflected. In addition, sunglint revealed what appear to be atmospheric gravity waves downwind of many of the Aegean Islands.

NASA MODIS Sunglint Annotated

July 3, 2014

While sunglint often produces visually-stunning images, the phenomenon can create problems for remote sensing scientists because it obscures features that are usually visible. This is particularly true for oceanographers who use satellites to study phytoplankton and ocean color. As a result, researchers have developed several methods to screen sunglint-contaminated imagery out of data archives.

Despite the challenges posed by sunglint, the phenomenon does offer some unique scientific opportunities. It makes it easier, for instance, to detect oil on the water surface, whether it is from natural oil seeps or human-caused oil spills. This is because a layer of oil smooths water surfaces.

NASA images courtesy LANCE/EOSDIS MODIS Rapid Response Team, GSFC.

1 Comment on "The Science of Sunglint"

  1. Clyde Spencer | October 9, 2021 at 3:51 pm | Reply

    “If you look frequently at satellite imagery or astronaut photography, you have probably noticed bright patches of light that can make certain bodies of water gleam with unusual color.”

    First of all, that should read “unusual brightness,” not “unusual color.” Although sunglint is always present, and is particularly strong near the Terminator, it is infrequently observed because most imaging satellites have nadir views (nearly straight downward). Sunglint occurs when the viewing angle is towards the sun and has the same angle as the angle of incidence of incoming rays.

    It should be obvious from the above pictures that the total reflectivity of the water is higher than the nominal or average reflectivity resulting from the low specular reflectance with small angles of incidence, and the added diffuse reflectance of sediment and plankton suspended in the water. Actually, the specular reflectance can reach 100% at the Terminator, giving a time-averaged specular reflectance of 12 to 18% for a parcel of sunlit water, depending on the latitude. This is considerably higher than the 6% value usually cited for open water!

    https://wattsupwiththat.com/2016/09/12/why-albedo-is-the-wrong-measure-of-reflectivity-for-modeling-climate/

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