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Like cream mixing in a cup of coffee, atmospheric winds swirl clouds into eye appealing patterns determined by mixing boundaries and turbulence. Note also the subtle iridescence at the bottom edge of the cloud created by diffraction of light through the cloud droplets.
We usually think of Sedona as "red rock country," which it is. But at dawn, sometimes nothing is red here except the sun.
Yesterday's post had a bit of color. I decided to up the ante today. Found this little beauty in a residential neighborhood in Kansas City.
The start of our new weather serie.
Cumulus Humilis clouds
Cumulus clouds mostly form as a result of localized pockets of warm air rising.
Cumulus humilis is the smallest form of cumulus clouds and results from relatively weak convection (humilis means humble in Latin). This produces clouds that generally have flat bases and small, rounded tops. Technically, a cumulus cloud is considered to be a humilis formation if it is wider than it is tall, as estimated by an observer on the ground. The height of these type of clouds is about 500 tot 1000 meter or 2000 to 3500 feet. It's unusual that rain falls out of these type of clouds.
Attention friends, we've got ourselves another one who'se taking our pictures, with a link to 500px, but not mentioning where it came from: www.flickr.com/photos/michaelhaupt/14632815455/in/photoli...: