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Hurricane Charley Aug. 2004

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Hurricane Charley Aug' 2004 – PowerPoint PPT presentation

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Title: Hurricane Charley Aug. 2004


1
Hurricane CharleyAug. 2004
  • Rapid Intensification and Trough Interaction
  • By Andy Latto

2
Objectives
  • What is trough interaction?
  • EFC Theory (Eddy Flux Convergence)
  • Potential Vorticity PV
  • Models incorporating and forecasting trough
    interaction.

3
Trough Interaction
  • Dynamical and thermodynamic interaction between a
    hurricane vortex and upper level trough.
  • Trough needs to be close but not too close to
    storm for positive interaction (lt 400 to 1000km)
  • Trough acts as a catalyst and storm responds
    positively or negatively.

4
Trough Interaction Theories
  • EFC
  • PV 2 Added heating (omega) aloft forces a
    stronger thermal gradient below.
  • Enhanced outflow due to increase in upper level
    flow.
  • Potential Vorticity According to QG Theory,
    added positive vorticity advection increasing
    with height causes low level ascent.

5
Hurricane Charley
August 2004
6
Hurricane Charley
  • Rapid Intensification -24 hPa in 6 hours

7
Models Used
  • GFDL
  • AVN
  • Uses Axi-symmetic vortex
  • Adds in asymmetric vortex
  • Triple-nested movable mesh
  • 1/12 degree resolution
  • Good for hurricane intensity
  • Problems with initialization
  • Global Model
  • 100KM resolution
  • Good for synoptic scale flows
  • Bad for hurricane intensity

8
GFDL Aug . 12th 00Z Initialization
9
GFDL Aug 13th 06Z Initialization
10
GFDL Aug 13th 18Z Initialization
11
AVHRR imagery SST Aug 12th
12
GFDL Aug 13th 00Z Initialization
13
GFDL Aug 13th 00Z 18hr. forecast
14
AVN Aug 13th 6 hour forecast
15
GFDL Aug 13th 00Z 18hr forecast
16
GFDL Aug 13th 18Z initialization
17
AVN Aug 13th 00Z 18 hour forecast
18
Results / Conclusion
  • EFC and PV during trough interaction can either
    strengthen or weaken a TC
  • Excess vertical shear caused by either PV of EFC
    is negative factor for intensification. (Balance
    is important)
  • Rapid intensification of TCs is believed to need
    trough interaction, in part to occur.
  • Better data analysis, more offshore vertical
    data, and incorporation of data/equations into
    models necessary for accurate forecasting of
    trough interactions.
  • Lots theories at work here, and more work needs
    to be done to confirm these ideas.

19
ANY
  • QUESTIONS?????????????????????????????????????????
    ???
  • References are in typed paper
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