370 tropical
Download
1 / 68

370 Tropical - PowerPoint PPT Presentation


  • 138 Views
  • Uploaded on

370 Tropical. Trade Wind Inversion. Trade Wind or Subtropical Inversion. The height of the base of this inversion varies from about 500 m at the eastern extremities of the subtropical highs to about 2000 m at the western and equatorial extremities.

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about '370 Tropical' - vidor


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript


Trade wind or subtropical inversion l.jpg
Trade Wind or Subtropical Inversion

  • The height of the base of this inversion varies from about 500 m at the eastern extremities of the subtropical highs to about 2000 m at the western and equatorial extremities.

  • In the equatorial trough zone and over the western portions of the trade-wind belt, the inversion does not exist as a mean condition, although it appears in certain weather patterns.

  • The inversion is generally strongest when the height of its base is lowest, and vice versa. The thickness of the inversion layer varies from tens of m to more than 1000 m.

  • On the average its thickness is about 400 m.


Tropical analyses l.jpg
Tropical Analyses

  • See both midlatitude style, isobaric analysis, and streamline/isotach analyses.

  • Why the latter?



Monsoons l.jpg
Monsoons Tropics

A monsoon is a term from early Arabs called the "Mausin," or "the season of winds." This was in reference to the seasonally shifting winds in the Indian Ocean and surrounding regions, including the Arabian Sea.


Slide25 l.jpg

Indian Monsoon Tropics

SW US Monsoon



Saffir simpson scale remember these are sustained winds l.jpg
Saffir-Simpson Scale Tropics(remember: these are sustained winds)


Slide35 l.jpg

Their Origin Tropics


Hurricane prediction a mixed report l.jpg
Hurricane Prediction: A Mixed Report Tropics

  • During the past thirty years there has been substantial in improvement is hurricane track forecasts as computer models improved and more data became available to describe their environment.

  • Over the same period only minimal improvement is hurricane intensity forecasts.


Slide43 l.jpg
Better synoptic forecasts and more information in the environment of these storms have aided prediction of their tracks


Substantial promise l.jpg
Substantial Promise environment of these storms have aided prediction of their tracks

  • The use of higher resolution prediction and more detailed data around and in hurricanes should result in better intensity predictions.

15-km grid spacing

1.67 km grid spacing


Slide48 l.jpg

Katrina environment of these storms have aided prediction of their tracks

48-h Before: Virtually a Perfect Forecast of Track


Katrina l.jpg
Katrina environment of these storms have aided prediction of their tracks

  • But the intensity was not well forecast until the day before….

  • Friday’s intensity prediction (storm hit Monday AM)

HURRICANE KATRINA DISCUSSION NUMBER 12

NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL

11 AM EDT FRI AUG 26 2005

FORECAST POSITIONS AND MAX WINDS

INITIAL 26/1500Z 25.1N 82.2W 70 KT

12HR VT 27/0000Z 25.2N 83.1W 75 KT

24HR VT 27/1200Z 25.5N 84.3W 80 KT

36HR VT 28/0000Z 26.2N 85.2W 85 KT

48HR VT 28/1200Z 27.1N 85.9W 90 KT

72HR VT 29/1200Z 29.5N 86.3W 100 KT

96HR VT 30/1200Z 34.5N 83.5W 35 KT...INLAND

120HR VT 31/1200Z 40.5N 77.0W 25 KT...DISSIPATING INLAND


Slide50 l.jpg

  • URGENT - WEATHER MESSAGE environment of these storms have aided prediction of their tracks

  • NATIONAL WEATHER SERVICE NEW ORLEANS LA

  • 1011 AM CDT SUN AUG 28 2005

  • ...DEVASTATING DAMAGE EXPECTED...

  • .HURRICANE KATRINA...A MOST POWERFUL HURRICANE WITH UNPRECEDENTED

  • STRENGTH...RIVALING THE INTENSITY OF HURRICANE CAMILLE OF 1969.

  • MOST OF THE AREA WILL BE UNINHABITABLE FOR WEEKS...PERHAPS LONGER. AT

  • LEAST ONE HALF OF WELL CONSTRUCTED HOMES WILL HAVE ROOF AND WALL

  • FAILURE. THE MAJORITY OF INDUSTRIAL BUILDINGS WILL BECOME NON FUNCTIONAL.

  • PARTIAL TO COMPLETE WALL AND ROOF FAILURE IS EXPECTED. ALL WOOD

  • FRAMED LOW RISING APARTMENT BUILDINGS WILL BE DESTROYED. CONCRETE

  • BLOCK LOW RISE APARTMENTS WILL SUSTAIN MAJOR DAMAGE...INCLUDING SOME

  • WALL AND ROOF FAILURE.

  • HIGH RISE OFFICE AND APARTMENT BUILDINGS WILL SWAY DANGEROUSLY...A

  • FEW TO THE POINT OF TOTAL COLLAPSE. ALL WINDOWS WILL BLOW OUT.

  • AIRBORNE DEBRIS WILL BE WIDESPREAD...AND MAY INCLUDE HEAVY ITEMS SUCH

  • AS HOUSEHOLD APPLIANCES AND EVEN LIGHT VEHICLES. SPORT UTILITY

  • VEHICLES AND LIGHT TRUCKS WILL BE MOVED. THE BLOWN DEBRIS WILL CREATE

  • ADDITIONAL DESTRUCTION. PERSONS...PETS...AND LIVESTOCK EXPOSED TO THE

  • WINDS WILL FACE CERTAIN DEATH IF STRUCK.

  • POWER OUTAGES WILL LAST FOR WEEKS...AS MOST POWER POLES WILL BE DOWN

  • AND TRANSFORMERS DESTROYED. WATER SHORTAGES WILL MAKE HUMAN SUFFERING

  • INCREDIBLE BY MODERN STANDARDS.

  • THE VAST MAJORITY OF NATIVE TREES WILL BE SNAPPED OR UPROOTED. ONLY

  • THE HEARTIEST WILL REMAIN STANDING...BUT BE TOTALLY DEFOLIATED. FEW

  • CROPS WILL REMAIN. LIVESTOCK LEFT EXPOSED TO THE WINDS WILL BE

  • KILLED.


Slide51 l.jpg

Extratropical Transition environment of these storms have aided prediction of their tracks


Madden julian oscillation l.jpg
Madden Julian Oscillation environment of these storms have aided prediction of their tracks


Katrina64 l.jpg
Katrina environment of these storms have aided prediction of their tracks

  • 1833 deaths

  • 125 billion in damage


ad