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Well friends here we are, into our annual stint on the prime-time hurricane hot seat, that short six-week or so period of the total six-month season where we see more named storms develop than during the rest of the season combined. While we cannot over-emphasize the importance of being adequately prepared for the season, it is equally important to not get caught up in the "hurricane hype" (as I like to refer to it) that seems to permeate the airways each year by individuals with agendas that sometimes border more on the sensational than the logical.

As an example of this, I refer you to the practice of issuing these largely worthless forecasts for the exact total number of named storms that will develop. The reason I say "largely worthless" is not only because of the odds against hitting it right on the nose, but because it is not the number of storms that develop that is important. It is where these things eventually end up going that counts. For example, in 2005 the original prediction was for 13 named storms, yet we ended up with an unprecedented 28! However, out of those 28 storms, it was two (Katrina and Rita) in particular that everyone will remember, because it was those two that did the most damage, and of course in the case of Rita, scored a direct hit on our area. Then the very next year they predicted 17 and we ended up with only 9. So again I will repeat what I have always said….It takes only one storm to make for a very bad season, if that one storm makes a direct hit on our area. My advice is to prepare for each and every hurricane season as if this were the year our number was coming up, because you will not get a clue from these dubious full season forecasts.

I strongly recommend that you make a special effort to obtain a copy of our full-color tracking chart for a most comprehensive review of everything you need to know in order to prepare for these storms. You can find them at any one of the numerous branches of Cameron State Bank, located across the listening area, or at the KYKZ-96 studios.

I have included a few graphics here to make the visual understanding of the various stages of hurricane development easier to comprehend. The first stage is referred to as a "tropical wave," because as you can see on the chart, this is basically what it looks like when isobars (pressure strength lines) are applied to it. I have included arrows indicating the wind-flow within a wave. As you can see, the winds follow the pressure pattern, turning slightly inward towards the area of lowest pressure, but not completing a closed circulation (no west wind around the south side of the system). It looks a whole lot like any other low pressure trough you might see on the weather map, except for the fact that this one is deriving its primary energy off of the warm water temperature.

Tropical waves are a common everyday phenomenon in the tropics, and we should expect less than 10% of the over 100 that form in an average year

to go on and become full-blown storms. If a healthy tropical wave approaches our area from the east or southeast, east to northeast winds will precede it (see red arrows on chart), and then as the wave goes by, the majority of the rain will typically fall along and to the east of its axis, as winds come around to the southeast. Tropical waves can be troublemakers if they stall over an area and produce long training bands of thunderstorms, resulting in flooding. However, most simply enhance and organize our already present daily summer thunderstorm coverage as they go by.

If a tropical wave should happen to come under the center of an area of weak high pressure aloft, where the winds upstairs are diverging away from the center, then the thunderstorms building up within the wave will have an exit exhaust chimney aloft for the air in the top of the storms to move away from the wave, making way for new fresh air entering the wave at the bottom to lift up much faster. The faster the air lifts up at the bottom, the lower the pressure falls, and the lower the pressure falls, the faster new air coming towards the wave moves in. Once this is happening all the way around the wave, air begins to flow in from all directions as a common "closed off" area of low pressure develops, and the system receives its classification as a "tropical depression".

The basic trick to any further development requires that the upper level part of the system be moving along exactly in tandem with the lower part. If the wave outruns its support aloft, or the other way around, the winds aloft will begin to sheer off the precisely organized vertical shaft of rising air currents, and further development will be prevented, and the system may even dissipate, depending upon the severity of the sheer. This is the main reason why you do not see more tropical waves go on to become hurricanes (thank goodness). It takes a very exacting balance of conditions from the surface all the way up, acting in precise coordination with each other to pull off developing into a hurricane.

Tropical depressions can be big troublemakers, as many in the past here have come up into our area and stalled out, dumping drenching torrential flood producing rains on us. A tropical depression stalling out just south of Sabine Pass could set the stage for a very serious flood event here, with our area being on its wetter east side, and just far enough offshore not to be killed off by the landmass.

If all goes well for the depression and development continues until the circular winds around the center reach 39 mph, it graduates to "tropical storm" status and receives its name. The lower the pressure drops in the middle of the system, the faster the winds outside the system will rush in to try and equalize that pressure. Although tropical storm force winds can be a problem, primarily with tree damage and power outages, our past history here with tropical storms has definitely been biased more towards excessive heavy rainfall events. In fact, some of our all-time heaviest rains and resultant floods have come under the auspices of tropical storms. Tidal flooding along the coast has also proven to be a problem.

Once a tropical storm crosses that 74 mph threshold and becomes classified as a "hurricane," it has a chance to go down in history along with the Audreys, Andrews, Carlas, Camilles, and now Katrinas and Ritas of the past (although these super-storm names have been retired to the hall of fame and will never be used again). What happens here locally depends just as much upon the trajectory of the storm as it does its size and strength. Let's deal with size and strength first.

While everyone here in our area naturally makes comparisons to Audrey and Rita, it is wise to consider that a direct hit from a storm such as the gigantic Carla from 1961 or the category 5 Camille with gusts over 200 mph from 1969, or even worse yet, 1988's Gilbert, possessing both the tremendous size of Carla and strength of Camille at his height in the Caribbean, would reduce this whole area (not just Cameron) to a pile of rubbish. Gilbert still holds the all-time low-pressure record for any Atlantic hurricane at 26.13 inches of mercury. To put this in proper perspective for you, look at your home barometer, and chances are you will find this well below the bottom of the scale. A storm with that size and strength would send the storm surge far inland, even north of I-10, and major hurricane force winds much further north than that. Of course, what I am giving you here is a worst case scenario, highly unlikely to ever happen in our lifetime. However, the point to always remember is, although highly unlikely, it is certainly NOT out of the realm of possibility. It is all a matter of the roll of the dice. Remember this: Although Rita was certainly a major storm, it was by no means a worse case scenario.

Just as important as size and strength is the trajectory of the storm itself. Exactly where that eye comes inland makes all of the difference in the world as to what kind of weather we will experience. As my chart here shows, the NE quadrant is the most severe side of the storm. As a hurricane approaches us from the gulf, it usually (but not always) comes from a generally SE direction. If this is the case, then the first thing we here will notice will actually be a drying NE wind, which will lower the humidity and provide a deceptively pleasant but hot day ahead of the storm. Because of this sinking dry NE flow, you have to get much closer to the center of the storm on its west side to get into trouble than you do on its east side, where SE winds are feeding directly off the gulf into the storm

If you will remember, this dry hot NE breeze was exactly the weather we experienced here on Sept 22nd, as Rita made her initial approach, as everyone was making their escape in the great evacuation of our area, although of course we eventually ended up in the wet and most dangerous NE quadrant as she made landfall.

The weather is usually more dangerous in every respect further to the east of the eye than it is to the west. Of course, there is no way of knowing for sure which side of the eyewall we will be on in many instances (where a direct hit is forecast) because only a common minor last-minute wobble this way or that could make all of the difference in the world between just a nasty severe storm event, and a total disaster. Thankfully, the true nightmare experience is limited to just the relatively small eyewall area of the entire storm's circulation, and many people who brag about having been through a hurricane never really did experience the actual central eyewall part of the storm.

Another side-effect of a hurricane being given more emphasis recently (and rightfully so) is the tremendous release of torrential rain further inland that sometimes results in loss of life and property comparable to closer to the coast. Right here along the I-10 corridor, we could possibly find ourselves in the tragic position of having to deal with both tidal flooding and river flooding.

It would be nice if everyone could just somehow absorb the sense of total helplessness that those who have been through the heart of a major hurricane have felt, but unfortunately, for some reason it is human nature not to transpose the feelings of someone else's disaster to our own personal lives. This is very similar to the attitude most people have towards things like cancer and traffic accidents. You never really deep down inside believe it will happen to you till it does. This is why people still over-expose their skin to the sun, despite the mountains of evidence proving it leads to skin cancer. This is why people still refuse to fasten their seat belts, regardless of overwhelming statistics that show it leads to more serious injuries and death in traffic accidents. And, this is precisely why people procrastinate on hurricane preparedness, thinking that this is just something that happens to someone else. This is simply human nature, and I guess it keeps us from going through life in a state of paranoia.

Now that we have a direct hit from a major hurricane under our belts, I find that there seems to be two different attitudes prevailing around here. People are tending to either be overly paranoid about the prospects of possibly being hit again this year, or they have this attitude that since we have had our hurricane now, the odds are great that we will not have to worry about it again this year. The truth is, the advent of Rita neither increases nor decreases our chances of being hit again this year. It is strictly a roll of the dice each year. The best thing you can do is coolly and calmly prepare for the season as if our number were coming up again, and then don't lose any sleep over it until something looks like it might get close enough to threaten us.

In my next commentary I will present a sneak preview into the upcoming fall season. As always, thanks again for your continued support.
 

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