Paul Knightley
EF5
Well, now I've started to get the YouTube bug - here's a timelapse of the huge gust front over NW Oklahoma on May 27th, 2001...near Shattuck.
http://www.youtube.com/watch?v=RqqCESro-rc
For those who do not know the set-up that day:
Initially, several supercells developed in Kansas, but with a NW'erly flow aloft and strong cold pool generation within the various cells they soon began to propogate south-eastwards. They raked much of Oklahoma with high winds, up to 100mph in places, and rain/hail.
What you can see here is the RFD of an HP supercell, and at times (e.g. at the start), you can see the "notch" where inflow is going into the supercell. The video ends as the gust front is about to pass over - we legged it south and end, but it caught up with us at Arnett, and we experienced high winds and heavy rain. The laminar look is because the boundary layer is generally stable, and as it's lifted up over the colder wedge of rain cooled air the moisture condenses just like with a lenticular cloud. It is then further lifted until it reaches its level of free convection and then explodes upwards as the storm.
http://www.youtube.com/watch?v=RqqCESro-rc
For those who do not know the set-up that day:
Initially, several supercells developed in Kansas, but with a NW'erly flow aloft and strong cold pool generation within the various cells they soon began to propogate south-eastwards. They raked much of Oklahoma with high winds, up to 100mph in places, and rain/hail.
What you can see here is the RFD of an HP supercell, and at times (e.g. at the start), you can see the "notch" where inflow is going into the supercell. The video ends as the gust front is about to pass over - we legged it south and end, but it caught up with us at Arnett, and we experienced high winds and heavy rain. The laminar look is because the boundary layer is generally stable, and as it's lifted up over the colder wedge of rain cooled air the moisture condenses just like with a lenticular cloud. It is then further lifted until it reaches its level of free convection and then explodes upwards as the storm.