Current Radar or Satellite Image

Flhurricane.com - Central Florida Hurricane Center - Tracking Storms since 199531 Years of Hurricanes Without the Hype - Since 1995


POLO LANDFALLS IN MX. TROPICAL STORM CONDITIONS POSSIBLE IN SW US TUES PM/WED AM. HISTORIC MULTI-STATE MULTI-DAY MODERATE RISK FOR FLOODING UNDERWAY.
Days since last Hurricane Landfall — US Any: 719 (Milton), US Major: 719 (Milton), FL Any: 719 (Milton), FL Major: 719 (Milton)
FlHurricane Atlantic Tropical Cyclone Tracking 🌀 Since 1995
23.7N -48.2W
Wind: 30MPH
Pres: 1011mb
Moving:
Present movement...wsw or 240 degrees at 12 mph...19 km/h
Click for Storm Spotlight
34.0N -44.5W
Wind: 40MPH
Pres: 1005mb
Moving:
Present movement...se or 125 degrees at 12 mph...19 km/h
Click for Storm Spotlight
HypeScale:
4.00
0510
Communication
Storm Data
Content
Follow & Connect
 


General Discussion >> Hurricane Ask/Tell

Pages: 1
Jamiewx
Storm Tracker


Reged:
Posts: 371
Loc: Orlando, Florida
Divergence and Vorticity
      #15302 - Sat Jun 12 2004 10:40 PM

Hey Guys

Is there anyone that can explain what Divergence and Vorticity is and how it affects tropical cyclones. I see maps online all the time and don't how to use them


Post Extras: Print Post   Remind Me!   Notify Moderator  
HanKFranK
User


Reged:
Posts: 1841
Loc: Graniteville, SC
Re: Divergence and Vorticity [Re: Jamiewx]
      #15386 - Sun Jun 13 2004 10:28 PM

i can give you an idea.. may be 'right' but probably not on the money, scientifically.
vorticity is sort of like angular momentum, but in a fluid... in this case air. it's the tendency for something to continue gyrating, a ripple of lower pressure in the atmosphere with coriolis deflection working on it. it isn't necessarily a closed, circular turning, it may just show as a 'hook' in the wind field. a vorticity maximum is often the focal point for a developing tropical system.
divergence is a 'split' in an air current. when we're thinking of it in terms of tropical weather, it's the stuff happening at high altitudes, jet stream level (around 200mb for instance). when you have a forking in the upper air currents, the air below rises to take its place, think of it sort of like a siphon working on the air parcel below. i'm not sure if you'd call it dynamic forcing. anyway, rising air condenses, usually feeds convection, provides proper ventilation. it can work as a makeshift outflow jet for a developing tropical cyclone.. thats why the location and track of the system relative to the upper air flow is so important.. upper air winds can work for a tropical system (divergence or an outflow jet) or against (wind shear), and have a great deal of the influence in steering most tropical systems.
hope you can use some of that...
HF 0229z14june


Post Extras: Print Post   Remind Me!   Notify Moderator  
Pages: 1



Extra information
0 registered and 0 anonymous users are browsing this forum.

Moderator:  CFHC, Ed Dunham, Colleen A., danielw, Clark, RedingtonBeachGuy, Bloodstar, tpratch, typhoon_tip, cieldumort 

Print Topic

Forum Permissions
      You cannot start new topics
      You cannot reply to topics
      HTML is disabled
      UBBCode is enabled

Rating:
Topic views: 5637

Rate this topic

Jump to