Snell's window

Snell's window (also called Snell's circle^[1] or optical man-hole^[2]) is a phenomenon by which an underwater viewer sees everything above the surface through a cone of light of width of about 96 degrees.^[3] This phenomenon is caused by refraction of light entering water, and is governed by Snell's Law.^[4] The area outside Snell's window will either be completely dark or show a reflection of underwater objects by total internal reflection.

Underwater photographers sometimes compose photographs from below such that their subjects fall inside Snell's window, which backlights and focuses attention on the subjects.

Image formation

Image one: light coming up from the water at a steep angle passes through, bent outwards away from the vertical. Image two:light hitting the surface at the critical angle is bent to pass along the water's surface. Image three: light hitting the surface at a shallower-than-critical angle cannot pass; it is reflected back into the water.

Refraction of light at the interface between two media, including total internal reflection. Looking straight up, one can see above the surface; looking at a flat angle, one can only see a reflection of the bottom of the water.

View straight up from underwater. The above-water hemisphere is visible, compressed (as by a circular fisheye lens) into a circle (Snell's window) bounded by the critical angle. Everything outside the critical-angle circle is reflected from below the water.

Under ideal conditions, an observer looking up at the water surface from underneath sees a perfectly circular image of the entire above-water hemisphere—from horizon to horizon. Due to refraction at the air/water boundary, Snell's window compresses a 180° angle of view above water to a 97° angle of view below water, similar to the effect of a fisheye lens. The brightness of this image falls off to nothing at the circumference/horizon because more of the incident light at low grazing angles is reflected rather than refracted (see Fresnel equations). Refraction is very sensitive to any irregularities in the flatness of the surface (such as ripples or waves), which will cause local distortions or complete disintegration of the image. Turbidity in the water will veil the image behind a cloud of scattered light.

References

^ Dave Hughes (1990). Tactics for Trout. Stackpole Books. ISBN 0-8117-2403-4. Snell's circle.
^ David K. Lynch and William Livingstone (2001). Color and Light in Nature. Cambridge University Press. p. 79. ISBN 0-521-77504-3.
^ Martin Edge and Ian Turner (1999). The Underwater Photographer. Focal Press. ISBN 0-240-51581-1.
^ Robert Williams Wood (1914). Physical Optics. The Macmillan Company. p. 66. circle-of-light water critical-angle 180.

External links

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[1] Dave Hughes (1990). Tactics for Trout. Stackpole Books. ISBN 0-8117-2403-4. Snell's circle.

[2] David K. Lynch and William Livingstone (2001). Color and Light in Nature. Cambridge University Press. p. 79. ISBN 0-521-77504-3.

[3] Martin Edge and Ian Turner (1999). The Underwater Photographer. Focal Press. ISBN 0-240-51581-1.

[4] Robert Williams Wood (1914). Physical Optics. The Macmillan Company. p. 66. circle-of-light water critical-angle 180.

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