NWS – National Hurricane Center

NWS – Tallahassee

NWS – Jacksonville

NWS – Melbourne

NWS – Tampa Bay

NWS – Miami

NWS – Key West

Saharan air layer analysis graphic

Data Courtesy of The NWS

Preliminary Local Climatological DataNaples
(WS FORM: F-6)Fort Lauderdale
 Fort Lauderdale Executive Airport
 North Perry Airport
 Opa-Locka Airport
 West Palm Beach
 Pompano Beach Airpark
 Tamiami Executive Airport
Climate SummaryFort Lauderdale
 West Palm Beach
Misc.Area Forecast Discussion
 Coastal Hazard Message
 Coastal Waters Forecast for South Florida
 Fire Weather Planning Forecast for South Florida
 Hazardous Weather Outlook for South Florida
 Preliminary Local Storm Report
 Marine Weather Statement
 URGENT – Marine Weather Message
 Short Term Forecast
 URGENT – Weather Message
 Point Forecast Matrices
 Florida Temperature and Precipitation Table
 Mainland South Florida Temperature and Precipitation Table
 Tabular Forecast for South Florida
 Special Weather Statement
 Surf Zone Forecast for South Florida
 Zone Forecast Product for South Florida

This graphic highlights any tropical depressions, storms, or hurricanes that the NHC is issuing advisories on as well as invests or other weather systems discussed in the Tropical Weather Outlook (TWO) and the Tropical Weather Discussion.

Tropical Weather Outlook Tropical Weather Discussion

(Click image below to enlarge) (Click image below to enlarge)

Select a map type to view:

Saharan air layer analysis graphic

NOAA FAQ: About the Saharan Air Layer 5-day Flash Movie of SAL

Total Precipitable Water

This graphic shows the GFS forecast for sea level pressure and wind vectors out to 48 hours

12 Hour 24 Hour 36 Hour 48 Hour

NHC 24 hour surface forecast showing sea level pressure, tropical waves, and current systems.

Surge Exceedance / Surge Probabilities

NHC Experimental Marine Graphicast

CIRA – Probability of TC Formation

Atlantic Sea Surface Temperatures (Click image for loop)

Click here for the latest Atlantic SST Anomalys

Wind Shear Analysis

(Click images for larger version)

Wind shear is a change in wind velocity (speed and/or direction) with height. Shear can rip a tropical cyclone apart or keep one from forming by preventing the convection from building. The following images show the latest wind shear and the shear tendency – whether it is increasing or decreasing.

This chart represents the 24-hour change in wind shear (shear tendency).

Upper level divergence is when the air in the upper levels of the atmosphere is moving away from a common area. It can induce sustained updrafts and therefore provide the exhaust system for a tropical cyclone, allowing it to strengthen.

Lower level convergence is when the air in the lower levels of the atmosphere is coming together in a relatively small area – the opposite of divergence. Eventually, there is nowhere for the air to go but up.

The steering winds in the atmosphere can help us determine the path and speed of a tropical cyclone. One rule of thumb says that the cyclone will move in the direction of the steering currents, but at about half the speed. However, the steering layer we need to look at is based on how deep the tropical cyclone is. We can determine this from the minimum pressure and then use the appropriate image below.

Steering Layer (MSLP 1000-1010mb))

Steering Layer (MSLP 990-999mb)

Steering Layer (MSLP 970-989mb)

Steering Layer (MSLP 950-969mb)

Steering Layer (MSLP 940-949mb)

Steering Layer (MSLP 940mb or less)