While waiting for her train this morning at the Glen Cove train station in Long Island, NY, Amanda Curtis grabbed her phone and snapped a photo of an incredibly rare atmospheric phenomenon: A quadruple rainbow.
But, in the interview posted below, Curtis told The Weather Channel the image was authentic and taken in the open air:
At first we thought this quadruple rainbow picture was fake, but then we were blown away.For more amazing weather stories, check out the AMHQ with Sam Champion page on Facebook.
Posted by The Weather Channel on Tuesday, April 21, 2015
The photo was convincing to Paul Neiman, who works as a research meteorologist at NOAA’s Earth System Research Observatory. He posted this very helpful explanation on his Facebook page, which he allowed me to republish:
This is an outstanding example of a primary and secondary rainbow (relatively common) occurring together with their reflected-light counterparts (quite rare). Allow me to elaborate.A typical primary rainbow is caused by refraction and one internal reflection of sunlight within raindrops, resulting in a rainbow that is positioned 41 arc degrees from the anti-solar point (i.e., the point directly opposite the sun – for example, if the sun is 10 degrees above the horizon at your back, the anti-solar point is 10 degrees below the horizon directly in front of you). The refraction causes the separation of white sunlight into its component colors, with red on the outside of the rainbow and violet on the inside.The secondary rainbow, which is centered 51 arc degrees from the anti-solar point (i.e., the larger of the two bows during a typical display), involves two internal reflections of sunlight within the raindrops rather than one, resulting in a reversal of the color sequence (red on the inside and violet on the outside). We can usually only see the portion of these rainbows above the horizon, because there isn’t a sufficient density of raindrops between the observer and the ground to see the rainbow below the horizon (exceptions include full-circle rainbows viewed from locales such as airplanes and mountain tops).So far, so good. For the much rarer reflected-light rainbows shown in this spectacular photo, a large glassy-smooth water surface is required behind the observer. This smooth water surface reflects the sun, such that a second solar light source is generated. This reflected sun, which is located the same the number of arc degrees below the horizon as the real sun is above the horizon, creates a second primary and secondary rainbow on the opposite side of the sky from the sun, but with the center of these reflected-light rainbows above the horizon. The geometry dictates that the regular and reflected-light rainbows will join at the horizon, as this photo shows.
Neiman’s explanation requires a body of water to be behind the observer. And, indeed, Oyster Bay – located about 2 miles east-northeast of the train station “likely provided the reflective surface to create the reflected-light rainbows”, he said.
Neiman said he was “awe-struck by this photo”, so too apparently were the thousands who shared it on social media.