Cloud Stalker: A little preview

Tuesday, June 19, 2007

A little preview

Coming in December at 10pm Tuesday nights on We channel, will be the reality show The twister sisters.That is the show I, yes me will be on. I have a little sample I made of the best day I had.

I had the best time ever that day and cant wait to do it again!!

Spotting in my area has been a bust, I'm seriously thinking moving to the sea breeze boundaries so i can spot some real weather...
Today is overcast with yes chances of thunderstorms, for us here on the west coast of Pasco...Good luck!!Its funny at work they say " hey weather girl bring us some rain" I tell them.. " I just try to forecast the rain i'm not God" jeese!!
I hope you enjoyed my preview,I cant wait till the show airs!!I will definitely blog any changes in times and dates!! Have a good day and may a storm find its way to you!

3 comments:

Dewdrop said...: You had the complete experience. Lucky dog. We definitely have to go back, you and I!; June 19, 2007 at 10:43 AM
CloudStalker said...: oh we will, one day!!!; June 19, 2007 at 8:36 PM
Unknown said...: Here...I'm sure you'll appreciate this.

Original Productions When They Get Bored; October 21, 2007 at 11:14 PM

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HAIL (3/4 inch or greater)

Hail can cause significant damage to your vehicle, break windows and damage roofs of homes and businesses.
Hail can cause significant bodily injuries such as broken bones and even blindness if wind blown.
Softball (4.5 inches) sized hail was reported in Lake Wales, Florida on March 30, 1996.
Haildrifts, up to four feet deep of dime to nickel sized hail, occurred in low-lying areas near Zephyrhills, Florida on January 29, 1997.
Hailstones the size of softballs can fall at speeds faster than 100 mph

supercell

Supercells derive their rotation through tilting of horizontal vorticity (an invisible horizontal vortex) caused by wind shear. Strong updrafts lift the air turning about a horizontal axis and cause this air to turn about a vertical axis. This forms the deep rotating updraft, the mesocyclone.
A cap or capping inversion is usually required to form a downdraft of sufficient strength. The cap puts an inverted (warm-above-cold) layer above a normal (cold-above-warm) boundary layer, and by preventing warm surface air from sinking too far, allows one or both of the following:
Air below the cap warms and/or becomes more moist
Air above the cap cools
This creates a warmer, moister layer below a cooler layer, which is increasingly unstable (because warm air is less dense and tends to rise). When the cap weakens or moves, explosive development follows.
In North America, supercells usually show up on Doppler radar as starting at a point or hook shape on the southwestern side, fanning out to the northeast. The heaviest precipitation is usually on the southwest side, ending abruptly short of the rain-free updraft base or main updraft (not visible to radar). The rear flank downdraft, or RFD, carries precipitation counterclockwise around the north and northwest side of the updraft base, producing a "hook echo" that indicates the presence of a mesocyclone.