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STORM CLOUDS WITH SILVER LINING
The 2006 Surf Atlantic Hurricane Prognosis


By:
Mike Cianciulli and Mike Watson 
April 14, 2006

The 2006 Atlantic Hurricane Season will go down as the most active year ever recorded. After all, who’d ever thought the NationalHurrican Surfing Weather Service would run out of storm names and resort to letters in the Greek alphabet? Then made it all the way to Zeta to boot!

<>Surely different folks were dealt assorted hands by the relentless storms. New Orleans took quite a bashing and residents have still not recovered as the 2006 season looms just six short weeks away. Surfers seemed to have mixed reviews depending on where they surfed.

“From Brian Hewitson to Peter Mendia, all the boys were saying how epic the Gulf was,” recalls Florida pro Will Tant. “But I booked three separate flights home to chase swells and never really scored.”
 

Foremost authority and hurricane forecasting pioneer Dr. William Gray, along with his right hand man, Phil Klotzbach, of Colorado State University, just released their predictions for 2006. Drum roll please… Put your money on 17 named Atlantic storms, with nine developing into full-blown hurricanes. But while the general public is understandably anxious to know precisely when and where storms will hit, Dr. Gray’s announced predictions are still no more than a mathematical formula, which often result in limited accuracy.

So we decided to ask Surfing Magazine Senior Editor Matt Walker, who calls the Outer Banks home, his take on the upcoming season. "It's almost statistically impossible to recreate last year. So, if I was going to make a prediction -- which isn't the smartest thing to do in this situation -- I see lots of pre-season hype and fear with comparatively little pay off."

But of course, Surfline fields the best surf forecasters in the world. While meteorologists can predict the storms, only surf forecasters can apply them to wave quality. Surfline’s East Coast forecaster, Mike Watson, notes that with this being a La Nina year (although a somewhat weak La Nina), one of the variables is in place that can potentially result in an increased number of storms in the Atlantic.

The La Nina phase - or cold phase - of the El Nino-Southern Oscillation (ENSO) dishes out weaker wind shear for the Atlantic Basin. A strong wind shear almost always results in the death of tropical cyclones. Conversely, reduced wind shear over the Atlantic basin (as a result of La Nina) affords a better opportunity for tropical cyclones to develop and/or maintain intensity.

The other variable that hints at potentially more storms is the continued warmth of the Atlantic Ocean waters. These warm waters are the fuel necessary for tropical cyclones. 

But there are a few wild-card possibilities that still lurk and could throw Dr. Gray’s prediction off course. Although these variables are incorporated in Dr. Gray’s equation used to forecast the number of storms, the precise impacts are not fully known until the season unfolds.

<>"If I was going to make a prediction -- which isn't the smartest thing to do in this situation -- I see lots of pre-season hype and fear with comparatively little pay off."
                                                                                                ~ Matt Walker, Surfing Magazine Managing Editor  

First, there’s the African Easterly Jet (AEJ) – a mid level region of strong winds for our African easterly waves normally located around 11° N latitude along the west coast of Africa. The exact location and shape of this jet can either make or break a season. If the jet is located too far south, the easterly waves coming off of the African coast may not have enough instability to produce a weather system. Furthermore, instability and storm formation tend to favor more sharply curved jets, thus a broadly shaped AEJ may also hinder chances for storm formation. For example, in 1997, a down year for storm formation in the Atlantic, we saw a southward-located and broad AEJ. Contrarily, in 1995, which was a very active season, we saw a sharply curved jet located north of what would be expected on average.

There’s also the Saharan Air Layer (SAL) – a dry, dusty air mass. This inhibits storm growth or can cause systems to weaken if this air becomes entrained in the system. These are monitored by satellite during the season. This means we can watch some of this dust make its way across the ocean, sometimes leaving a fine layer of dust on vehicles as far away as Florida. In fact, there are instruments in place in Florida to measure just how much of this dust makes its way across the Atlantic.

Finally, the exact position of the sub tropical high pressure (STHP), otherwise known as the Bermuda high,
Atlantic anti-cyclonic gyre, among other aliases, has been parked close to home the past couple of seasons. With the high-pressure center located close to North America the past two years, we have seen storms steered into our coasts instead of moving harmlessly into theAzoresAtlantic. This actually appears to be more the norm than the exception. The landfall totals by state tell the tale, with Florida recording a whopping 10 strikes over 18 months. Look back over the last 100 years and the numbers are even more staggering.

These are only a few of many variables that go into predicting the number of storms for any given season. While the amount of storms called for this year is dramatically less than gyrated throughout Atlantic last year, it always pays to be prepared. And remember, there's not that much time left: The 2006 season officially kicks off June 1.
 


Story courtesy of Surfline.com