Atmospheric refraction can create fascinating optical phenomena, as captured in Jim Grant's sequence of sunset images from north of San Diego. These images showcase a range of effects, including looming, towering, mock mirages, and the elusive green flash. By understanding the underlying principles of refraction, we can unravel the mysteries behind these captivating phenomena.
In Grant's photographs, the distorted appearance of the sun and the presence of a green flash at its upper limb are both attributed to refraction caused by multiple stacked temperature inversion layers. These layers consist of kinks in the normal fall in air temperature with height, with warmer air situated above cooler air. Notably, there are at least two inversion layers at play here.
Looming is an age-old term used by sailors to describe the phenomenon where distant objects that should be below the horizon appear raised up. In the case of Grant's images, the visibility of San Clemente Island, located 70 miles away, can be attributed to relatively cool air beneath the lowest inversion layer. This cooler air, combined with a normal temperature gradient, causes the island to loom above the horizon.
While looming raises objects without distorting them, something more intriguing is happening to San Clemente Island in Grant's photographs. The island's image appears distorted, with its peaks stretched vertically. Sailors referred to this phenomenon as towering. The distortion is likely a result of the lowest temperature inversion, which reduces or even reverses the vertical temperature gradient towards the top of the island profile. As a result, the island image is stretched more at its top than at its lower part.
While looming and towering are both distortions resulting from atmospheric refraction, they are distinct from mirages. Mirages require the presence of inverted or multiple images, which are absent in these phenomena. Therefore, the images captured by Grant exhibit the characteristics of looming and towering rather than mirages.
The captivating images captured by Jim Grant are not the only instances where looming and towering can be observed. Additional photographs showcase these atmospheric refraction effects in different settings, providing further insight into their occurrence.
Among the various atmospheric refraction effects, the green flash stands out as a particularly elusive phenomenon. This optical phenomenon occurs during sunrise or sunset when a brief green light appears on the upper rim of the sun. While challenging to observe due to its fleeting nature, Grant's images offer a glimpse of this captivating event.
Jim Grant's sequence of sunset images provides a captivating exploration of atmospheric refraction effects, including looming, towering, mock mirages, and the elusive green flash. By delving into the principles behind these phenomena, we gain a deeper understanding of the ways in which our atmosphere can distort and transform our perception of the world around us. These optical wonders continue to inspire awe and curiosity, reminding us of the intricate and mesmerizing nature of our atmosphere.
Looming, Towering, Mock Mirage, Green Flash ~ Jim Grant�s sequence of sunset images from north of San Diego show all these atmospheric refraction effects. Notably, San Clemente Island some 70 miles away is visible with a definitely non-realistic mountain profile. ©Jim Grant, shown with permission.
The distorted sun and the green flash at its upper limb result from refraction by several stacked temperature inversion layers � kinks in the normal fall in air temperature with height with abnormally warmer air above cooler. There are at least two inversion layers.
Looming is an old sailors' term. Distant objects that sometimes should be below the horizon appear raised up. Here the appearance of 70 mile distant San Clemente is due to the combination of relatively cool (and normal temperature gradient) air beneath the lowest inversion layer.
Looming does not distort a distant object, it merely raises it. But something more is apparently happening to San Clemente because the island does not have such steep conical peaks! Sailors called this towering. The island image is distorted - stretched vertically. The towering is probably a result of the lowest temperature inversion which reduces or even inverts the vertical temperature gradient towards the top of the island profile. In effect the island image is stretched by more looming at its top than at its lower part.
Looming and towering are distortions from atmospheric refraction but not mirages. They lack the inverted or multiple images necessary for them to be called mirages.
More looming & towering
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"OPOD - Looming, Towering, Mock-Mirage, Green Flash". Atmospheric Optics. Accessed on November 21, 2024. https://atoptics.co.uk/blog/opod-looming-towering-mock-mirage-green-flash/.
"OPOD - Looming, Towering, Mock-Mirage, Green Flash". Atmospheric Optics, https://atoptics.co.uk/blog/opod-looming-towering-mock-mirage-green-flash/. Accessed 21 November, 2024
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