Cloud Stalker: Happy 20th anniversary of my daughter's birth

Thursday, March 6, 2008

Happy 20th anniversary of my daughter's birth

March 7th 1988 at 1:13 am my daughter was born. Twenty i can't believe it years ago,holy crap man i have a child in her 20's. 20 great years she was my life for so long and now she has her own i guess now i look forward to grandchildren. ( Insert laugh) i can wait awhile on that i do still have a seven year old. Happy Birthday Binners!!I love you!!!

15% chance of severe storms tomorrow(Today).MODEL DATA STILL SUGGESTS STRONG LOW LEVEL WINDS IN THE FRIDAY
AFTERNOON THROUGH SATURDAY EARLY MORNING HOURS JUST NORTH OF THE
AREA WHICH MAY PROVIDE ADDITIONAL DYNAMIC SUPPORT SOME SOME
THUNDERSTORMS TO BECOME SEVERE...ESPECIALLY NORTH OF THE TAMPA BAY
AREA. Of course i have to work, im not liking working nights but at least i am working. I am so tired, I will post more tomorrow.
night,
Jess

2 comments:

Dewdrop said...: Happy Birthday to your daughter!!!; March 7, 2008 at 11:32 AM
CloudStalker said...: Thanks Dew!!!; March 7, 2008 at 10:45 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.