Cloud Stalker: fighting to live/TS Ingrid

Friday, September 14, 2007

fighting to live/TS Ingrid

Well she made it, barely but she is now a storm. Will it become more? It really doesn't look like it with all the shearing that lies ahead check it out...

I will be keeping my eyes on it, but i don't hold any hope for her. Its a ruff sea out there right now.
In my neck of the woods it looks like another typical summer day again it looks like the west coast seabreeze will keep most storms off the coast(coastal drought) I think i need to move more inland...lol

Last night i watch from a distance the clouds being lit up, by the time it reach me i was sound to sleep. .26" rain so i didn't miss much.
well i gotta go earn some dough, I will post if by any chance i can get out for an easterly chase today, my mom is coming over so chances are i will be stuck here:( but one never knows.....Happy Friday and remember KEEP THOSE EYES TO THE SKY!!!JESS

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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.