Tuesday, January 29, 2013

KELVIN-HELMHOLTZ WAVES


Those aren’t ocean waves in the photo but are a cloud form known as Kelvin-Helmholtz waves (aka shear-gravity clouds or KHI clouds), named for Lord Kelvin and Hermann von Helmholtz. Kelvin-Helmholtz waves form when a fast layer moves over a slower layer, dragging the top along to create a curled shape. The swirling eddies at the top of the cloud layers are usually evenly spaced. Sea waves break when their bases slow down upon reaching shallow water and their crests surge ahead. Cloud waves ‘break’ in a similar fashion; when their crests are pushed ahead of their troughs by the difference in air currents.

If the differences between the air speed and the temperatures of the layers of the atmosphere are small they will glide over each other. If the difference between the layers is too great then where the layers meet turns into turbulence. When the atmospheric conditions between the two layers are just right, Kelvin-Helmholtz waves form. The example in the photo is one where the air between the two atmospheric layers is close to the threshold for turbulence.

The photo was taken from the Alabama Air National Guard facility at the Birmingham-Shuttlesworth International Airport, in December 2011. The Kelvin-Helmholtz waves seen in Alabama occurred when there was a cold layer of air near the ground, where the wind speed is low. A warmer and faster moving layer of air was probably moving over this cold and slow-moving layer.

Animation of Kelvin Helmholtz Instability:http://bit.ly/11lJQS7
Vortex formation in free jet caused by Kelvin-Helmholtz instability: http://bit.ly/VlnEmS

Video of the Kelvin-Helmholtz wave clouds over Birmingham: http://bit.ly/tjtWWG


More cloud photos and information here: http://cloudappreciationsociety.org/,https://www.facebook.com/cloudappreciationsociety?ref=ts&fref=ts

http://weather.about.com/od/cloudsandprecipitation/p/KelvinHelmholtz.htmhttp://dvice.com/archives/2011/12/strange-tsunami.php
Image credit: ABC 33/40 in Birmingham, Alabama



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