Fractocumulus from Above
The deep troposphere behind a convective complex often can be a richly layered melange of clouds. This was no exception. A broad area of outflow covered central and eastern Oklahoma from overnight thunderstorm clusters, scud (fractocumulus) in the rain-cooled boundary layer wafted across the area from the southeast, while streamers of altocumulus and a deck of anvil-residue cirrostratus layered the skies above. After takeoff from OKC airport, all became visible at once.
over Oklahoma City OK (13 Jun 15) Looking NW