This educational section is for an in-depth view of one of nature's most powerful storms: TROPICAL CYCLONES! These storms are those whirlpools that develop each tropical season over the tropics, what we call "hurricanes" in the Atlantic and East pacific and "typhoons" in the West Pacific. These storms have a very special place in the meteorological world and will be explained in great detail in this section. Note - This page may take a while to load on some SLOWER connections! |
Tropical Wave: This is a low pressure trough (a non-closed low pressure area) moving through the trade winds over the tropical ocean. As many as 100 of such waves (also called inverted troughs, because of their "upside down" appearance on a tropical weather map in the northern hemisphere) move across the tropical Atlantic during the hurricane season for that region, which lasts from June 1 to November 30. Sometimes, such tropical waves can develop enhanced showers and thunderstorms, creating a low pressure area that can further develop into a tropical cyclone (such as a tropical depression or even a tropical storm). On average, about six of such tropical waves go on to becoming a "named" tropical cyclone (tropical storm status or greater) during each Atlantic hurricane season. In the annotated satellite picture, the yellow arrows show a northeast wind ahead of the westward (left) moving wave then a southeast wind behind the convergence line. Since no westerly winds yet exist south of the system, the tropical wave is basically an "open" or "north-south" axis of low pressure (a trough). | |
Tropical Disturbance: This is a weak or broad area of low pressure. It can be associated with a developing tropical wave or within a developing area of convection over the tropical ocean. This is a cluster of convective clouds (showers and thunderstorms) that has become persistant and has the potential to develop into a tropical depression. Winds within such a system are normally well under 25-30 MPH. Persistant tropical convection tends to lower surface pressures (called a CONVECTIVE VORTEX), and is vital to tropical cyclone formation under the right conditions (warm sea surface, minimal upper-level wind shear, etc). Besides developing along a tropical wave, tropical broad lows can also form along stalled frontal systems, even remnants of previous tropical storms. | |
Tropical Depression: This is a tropical cyclone with winds of over 30-MPH but less than 38-MPH. A tropical depression must be a CLOSED low pressure area (at least one closed isobar on a 2-MB pressure interval weather map) to be classified as such. This is the first major stage in tropical cyclone / tropical storm formation. | |
Tropical Storm: Is then the maximum sustained winds (a one-minute mean windspeed at sea level) in a tropical cyclone reaches 38-MPH but less than 74-MPH. The tropical storm usually has well-developed closed cyclonic circulation. Tropical storms are the stage inwhich the tropical cyclone is given a name from a list of names unique to the area that tropical cyclone developed in. In the Atlantic basin, an alphabetic list of alternating male and female first names is used that repeats every six years. A major hurricane or storm that causes exceptional damage and / or loss of life is usually removed from the list and replaced with a new one to avoid confusion 6 years later. | |
Hurricane: This is the most intense stage of tropical cyclone development. The term "hurricane" (or other name such as "Willy-Willy" in Australia and "typhoon" in the west Pacific) is applied to any tropical cyclone with winds at or over 74-MPH. Hurricanes (called so in the East Pacific and Atlantic) are derived from an Indian name for "bad winds", and represent a tropical cyclone with an intense closed cyclonic wind flow and pressure structure. Once at the hurricane stage, the tropical cyclone is now classified by its destructive power on what is the SAFFIR-SIMPSON scale, rating the storm based on how much damage its winds can do on a scale from 1 to 5. The highest winds ever measured in a hurricane or typhoon have exceeded 200-MPH. | |
Extratropical Storm: As a hurricane, typhoon, tropical storm, or any tropical cyclone enters the higher (temperate) lattitudes, it begins interacting with the increased temperature gradient as you go from south to north (or north to south in the southern hemisphere). This is where cool, drier air is brought in on one side of the dying tropical cyclone and warmer air is brought in on the opposite side. In the annotated picture, a tropical cyclone has evolved to an extratropical (frontal) system. To its west, cool air had formed a cold front, while warm air surges north east of the remnant low pressure. Note the thunderstorm line along the cold front and drier air "punch" to its west. These extratropical (or even subtropical "hybrid" - as described in the next section) type stages do not always mean the storm is "weakening", but simply "changing" in response to a different environment it was introduced into. In the past, hybrid or extratropical storms of tropical cyclone orgins have caused exceptional flooding events (Such as Agnes in 1974) even wind and / or coastal damage events (such as "The Perfect Storm" in 1991). |
A "hybrid" (or subtropical) cyclone is a low pressure system that has BOTH the attributes of a frontal system (extratropical or wave cyclone) and a tropical cyclone (such as a hurricane). These attributes are rarely an exact "half and half" between the extratropical storms and their tropical cousins, but a rather involved and variable division of the two. For instance, tropical cyclones have a warm core, and extratropical cyclones have a cold core. The latter has fronts (cold and warm), but tropical cyclones do not. Tropical cyclones have feeder bands of convection, while extratropical cyclones have "waves" or frontal zones instead. The latter also develops in regions of high wind shear and / or high temperature gradients (such as in the temperate zone and is called BAROCLINICITY), while tropical cyclones favor light winds and little temperature gradients for development in tropical regions. Occasionally, and especially between the transitioning seasons (such as spring and fall) cyclones with BOTH characteristics form. They also account for only 2% of cyclone types (compared to tropical and extratropical storms). In the diagram above, a strong subtropical low develops off the SE USA / Florida coast. The first image (NWS and Weathertap.com) to the left is the water vapor image, showing a moist storm center and dry air all around it at high altitudes. One can easily make out where the low pressure center is. The middle picture (NCAR) is that of the surface winds and pressure. The large number of isobars denotes a strong pressure gradient, therefore strong winds (near 50 Knots). The last picture (FNMOC / US Navy) to the right shows the sea-state produced by the storm, with large ocean waves exceeding 20 feet in the normally calm waters (for the month of May) off the SE coast of the United States. Hybrid (subtropical) storms are often insidious when it comes to wind and wave damage. They are large, like an extratropical storm, but also have strong winds, much like a tropical system. Another bad example of a hybrid cyclone was the "perfect storm" around Halloween of 1991.
The two pictures above were taken from a webcam located on top of a sand transfer station on the north side of Lake Worth Inlet, which is on the south side of Singer Island in Palm Beach County, Florida during the morning of May 8. 2007. The provider of the webcam images is the town of Palm Beach (www.co.palm-beach.fl.us). In the two pictures, waves well over 15 feet are slamming into the jetty and breaking into the end of the inlet. This is also north of a very popular surf spot called "Reef Road". Note the wave run-up flooding inland along the side of the inlet in the left picture. These conditions are EXTREMELY dangerous for mariners and anyone standing too close to the breaking waves. Also note the deceptively blue skies and pleasant weather, which can lure beach-goers into a false sense of security, since the intense storm (hybrid cyclone) that is generating the large waves is hundreds of miles away.
In the three pictures above, the hybrid (subtropical) storm appears on visible satellite to the left and right for May 7, 2007 and May 8, 2007, respectively. One interesting change between the two pictures is that the left is much more "extratropical" in appearance, with a cold-front (or shear-axis) and well-defined dry-slot. However, to the right, the dry-slot is not as defined, and wraps completely around the storm. Also, more thunderstorms are developing around the storm center rather than along the fronts, forming almost a large and diffuse "eye" like feature. Sometimes, hybrid systems can "shift" their balance of attribute more towards extratropical cyclones (as in the left picture), or become more "tropical" like (as to the right). Sometimes they can make a full transition to one or the other altogether. Subtropical storms are an important area of interest because of their strange, and often intense character. The middle picture is a webcam shot of Boynton Inlet looking east, showing the large NE swells arriving at well over 10-12 feet. The provider of the webcam images is the town of Palm Beach (www.co.palm-beach.fl.us).
This diagram above is of three annotated images to show how vertical wind shear can quickly destroy a developing, or even a mature, tropical cyclone. First of all, in addition to warm water and many other factors, winds aloft need to be light to foster a good environment for a tropical system. Simply stated, the thunderstorm convection needs to remain over the SAME area as the developing low near sea surface. If the convection becomes detached from that surface low, the low simply "fills in" since the mechanism (convection) has been removed from it vertically.
Category One: Winds 74 to 95 MPH. Tree and shrub damage. damage to shingles. un-anchored mobile homes damaged. Storm surge about 3-5 feet. Damage to piers and boats. Examples: Irene in FL Keys in 1999, Gabrielle in FL in 2001, Erin in East-Central FL in 1995. | |
Category Two: Winds 96 to 110 MPH. Roof and window damage to buldings. heavy damage to trees and shrubs. heavy damage to mobile homes. Storm surge typically 5-8 feet. Boats and piers heavily damaged. Examples: Frances in East-Central FL in 2004, Isabel in NC in 2003, Lili in LA in 2002. | |
Category Three: Winds 111 to 130 MPH. Structural damage to buildings. Flying debris. Severe tree and shrub damage. Mobile homes destroyed. Storm surge typically about 8-12 feet. Storm surge destructive to any low lying coastal areas. Examples: Ivan in FL Panhandle in 2004, Gloria off NC in 1985, Betsy in FL in 1965. | |
Category Four: Winds 131 to 155 MPH. Extensive damage to most buildings, including complete wall and / or roof failures. Debris becomes deadly missiles. Major coastal flooding with damage and extreme beach erosion. Storm surge can be 12-18 feet. Examples: Charley in SW FL in 2004, Hugo in SC in 1989, Donna in FL in 1960. | |
Category Five: Winds at or above 156 MPH. Catastropic damage to many buildings, even re-inforced buildings receive major structural damage. Debris battering. Most roofs are blown off. Deforestation of wooded areas. Storm surge over 18 feet (maybe up to 25 feet, or more). Scouring of coastal structures. Category-five storms are very rare. Examples: Andrew in South FL in 1992, Gilbert in Carribean in 1988, Camille in MS in 1969. |
The Saffir-Simpson scale was developed by a former director of the National Hurricane Center and a structural engineer to rate a hurricane (or severe tropical cyclone) winds in terms of how much damage is done. This scale ONLY applies to tropical cyclones with winds at or over 74 MPH (hurricanes in the western hemisphere). This scale is the standard in hurricane forecasting eversince.
Note: There is one addendum I would like to add to this table about the Saffir-Simpson scale above ... Which is VERY important. The STORM SURGE heights shown are basically for an AVERAGE structured hurricane (25 mile-wide eye) with a fully-developed ocean state / wave envelope that has been nearly a steady-state, and affecting an average coastline. Smaller hurricanes can have a lower storm surge (as with hurricane Charley in 2004, where a storm surge of only 6-8 feet was present, despite 150-MPH category-4 winds). Larger hurricanes, or hurricanes that are rapidly weakening, can have a much larger storm surge despite weaker winds (such as Katrina in 2005 which had a 25 foot storm surge despite category 3 winds) ... This is very important to consider as coastline, sea floor topography, hurricane size, structure, and intensity trends can make the storm-surge versus category height guide practically useless!
The photo-composite diagram above is a picture of a "real" hurricane ("Elena" taken from the space shuttle in 1985) sliced in half showing its internal structure and annotated with labels and arrows showing wind flow. The graphic is NOT to scale. Most people are familiar of what a hurricane (or typhoon) looks like from high above, such as on a satellite picture. A large, white whirlpool of clouds with a "dot" in the center of it. The white swirl is merely the top of the storm, and alot more is going on under this "shield" of high clouds.
This diagram above is an annotated composite of two radar images of hurricanes Frances and Jeanne (the latter being more zoomed-in) just off the Florida East-Central coast on September 4, 2004 and September 25, 2004, respectively. In these radar images, both storms have a large eye (nearly 70 miles wide in Frances and 40 miles wide in Jeanne), however, only a single main eyewall surrounds the precipitation-free eye region.
This diagram above is an annotated composite of two radar images of hurricane Charley just before striking Punta Gorda, Florida on August 13, 2004. The image on the left shows the precipitation structure of the rather small, but extremely intense, hurricane. The core of the system (eye and eyewall) is circled and zommed in on the right image of the diagram. What is trying to be shown here is the DOUBLE EYEWALL, where a larger (but weaker) eyewall surrounds a smaller (but far more intense) inner eyewall. This phenomina is almost exclusively found only in major hurricanes (those with winds at or over 111 MPH). The inner eye is less than 5 miles wide while the outer eyewall is about 25 miles wide. A so called "moat" region of weaker radar echoes is between the two eyewalls.
The diagram above is two pictures taken by myself from inside the eyes of two hurricanes that hit the united states, hurricane Irene in Key West, FL in September 1999 to the left and devastating hurricane Charley in Punta Gorda, FL in August 2004 to the right. In the right picture, a brightening sky appears overhead and the opposite eyewall extends across the lower portion of the picture, causing what is called a "stadium effect". In the picture to the right, a much smaller eye presents a "tube effect" when viewed straight up with blue sky overhead.
The diagram above is a composite of two images, the left taken by a NOAA scientist aboard a WP3 "Orion" research aircraft (US Department of Commerce), while the image on the right taken by the US Air Force aboard a WC-130 "Hercules" aircraft (Military). Two of the images are unique in terms of what type of storm is being intercepted. The left picture is a major Atlantic hurricane with a large single eye, the right was taken between the outer and inner eyewalls of double-eyewall system hurricane Charley off SW Florida in August 2004.
Hurricanes and typhoons (tropical cyclones) can come in all shapes and sizes. The diagram above shows the immense differences in size of three tropical cyclones that broke records for size (measured across the breadth of the tropical storm forced, with speeds of 38-MPH or more, gale wind "envelope"). All storm examples are SCALE COMPARED to the continental United States to show the differences in their size. Most impressive is the size of super Typhoon "Tip", which formed in th west Pacific in October 1979. This tropical monster is also the strongest tropical cyclone on record, with winds sustained at over 190-MPH and a central pressure of 870 MB. Tip measured 1,200 miles across its envelope of gale-forced (38-MPH or more) winds, making it the largest tropical cyclone ever recorded. All statistics in the above diagram are as of early 2010.
The core regions or tropical cyclones, particularly the relatively clear eye and surrounding eyewall, also come in a variety of shapes and sizes. The typical eye diameter of a hurricane (or typhoon) is about 25 nautical miles. In the diagram above, two eye size extremes are shown, with Hurricane "Isabel" in 2003 (in the Atlantic Ocean) to the left, and hurricane "Wilma" in 2005 (in the Western Caribbean Sea). Both storms are category-five hurricanes, with wind speeds of 175 and 190 MPH, respectively (as of 2010, Hurricane Wilma was also the most intense tropical cyclone ever in the Atlantic basin, with a minimum pressure of 882 MB). The impressize difference is the eye diameters of the two storms. Isabel has a very large eye, over 70 nautical miles (NM) across, while Wilma's eye is less than 2 1/2 NM wide! Wilma set a record for the smallest eye ever observed in a tropical cyclone. The record for the largest eye was in Typhoon "Winnie" in the Pacific, with an eye diameter of nearly 230 NM!
This diagram above is an annotated composite of two satellite images. The image on the left denotes the important regions of a tropical cyclone relative to the storm's movement: The RIGHT-FRONT, RIGHT-REAR, LEFT-REAR, and LEFT-FRONT quadrants (in clockwise order). The important quadrants are labeled in white and separated by orange intersecting lines. The storm motion in this example is toward the upper-left (or northwest). The yellow arrows denote low-level inflow into the storm. The picture on the right also shows low-level inflow via yellow arrows but the importance of FEEDER BANDS, denoted by orange lines. Feeder bands are squall lines of showers and thunderstorms caused by lifting of air due to low-level CONVERGENCE. These lines of storms can be quite a distance from the actual "core" of the tropical cyclone.
The two images in the diagram above concern examples of actual and forecast tracks of tropical cyclones in the Atlantic basin. To the left is a screen snapshot from my own Visual BASIC program called "TChart 3.0" to track hurricanes with the 1995 Atlantic storm season's record-breaking tropical system tracks loaded. Each grey line represents a track for a tropical system, with the white tracking line being hurricane "Erin", which hit east-central Florida. As one can imagine, hurricane tracks seem "random" or taking on a "mind of their own". In actuality, tropical cyclones are embedded in a much larger and complicated flow in the atmosphere (from the easterly trade winds in the tropics through the westerlies of the higher lattitudes). Small disturbances within the atmosphere, such as high-pressure ridges and low-pressure troughs, are crucial to the path of tropical cyclones.
Strong Winds: The most obvious element in a hurricane (or any strong tropical cyclone) is the strong winds. Technically, any wind over gale forced (tropical storm forced begins at 38-MPH) can do damage by uprooting trees and damaging property. When winds reach 74-MPH or higher, damage increases radically, with each 50% increase in windspeed doubling the dynamic force of that wind. For example: A 75-MPH wind is TWICE as damaging as a 50-MPH wind, 100-MPH wind is FOUR-TIMES as damaging as 50-MPH, and a 150-MPH wind is NINE times as severe as 50-MPH! This is because the DRAG FORCE of wind, caused by aerodynamics and dynamic pressure of the wind flow, increases with a formula related to the SQUARE of the velocity. This is why a minimal hurricane with 75-MPH winds only causes leaf and minor tree damage but a hurricane like Andrew with 165-MPH winds back in 1992 can destroy an entire city. | |
Storm Surge: This is basically a dome or "mound" of water caused by the intense low pressure of a tropical cyclone coupled with the driving-force of the winds "pushing" the water along (mass transport). In deep water, the storm surge in intense tropical cyclones is only a foot or two high, caused by the low pressure, but contains a fast moving surface current called MASS TRANSPORT that flows with the storm winds (more enhanced to the right side of the storm core in the northern hemisphere). As this flow (and "mound") of water comes ashore, it interacts with the coastline, tides, and undersea topography and can be over 20 feet high in strong hurricanes! Storm surge rises quickly with the onset of the storm core and often floods coastal areas, threatening life by drowning, damaging beachfront property, marinas, even the coastline itself. Storm surge is most severe in and to the right (northern hemisphere) where the storm center crosses a coast. 90% of hurricane victims die from drowning in floods caused by the storm surge. | |
Heavy Rains: The rain bands and thunderstorms associated with a tropical cyclone, regardless of its wind intensity, are often heavy and accumulating. Such heavy rains can even occur well inland from weakening tropical systems, such as the incredible flooding from the remnants of hurricane Agnes (in NY) back in 1974. It is not uncommon for a tropical system to dump 10-15 inches of rain as it moves over a given area. Slow moving systems, such as hurricanes Irene (S FL) in 1999 and Mitch (Central America) in 1998 have dumped 20 to 30 inches of rain, respectively. Other tropical cyclones only dump a few inches of rain, especially if moving fast. Rain from tropical cyclones, especially hurricanes (referred to as "violent rain"), is nearly impossible to measure, because it falls "sideways" with the winds and "misses" the rain guages. I have seen wind blow water into a building wall "coating" it with several inches of water. Between gusts, when the wind let up briefly, all that water came cascading down at once in a waterfall! | |
Tornadoes: The spiral bands of a hurricane (or tropical cyclone) also have the capability to spawn tornadoes. Tornadoes can occur in any area of the tropical cyclone but the threat is much higher on the right-front side of the storm (northern hemisphere) because the low-level convergence and directional wind shear (helicity) is higher in that region of the storm. Often the leading rain bands spawn shallow MESOCYCLONES (rotating updrafts) that could produce a brief tornado, although these mini-supercells are much smaller than their "Great Plains cousins". Tornadoes can and have occurred in land-falling tropical systems (land creates more low-level drag and shear). Some tropical cyclones spawn more tornadoes than others, depending on the structure of the precipitation. There are even eyewall tornadoes (not to be confused with MINI-SWIRLS, which are simply eddies embedded in the eyewall winds). For example: Hurricane Beulah in 1967 spawned over 115 tornadoes! |
The diagram above is a model for the storm surge depicting AVERAGE height of the storm surge based on the Saffir-Simpson category of that storm (hurricane or typhoon) as well as the portions of a landfalling storm most suseptible to storm surge. The image to the left is a stock picture of South Beach, Florida with palm trees plus an image of myself used for comparison. The blue squares represent the height of a "model" surge relative to mean sea level (the beach was 3 feet above sea level where the picture was taken) in different category (1 to 5) intensity examples (5 being the highest to the left). As you can see, a category-1 hurricane (or typhoon) has the smallest surge, averaging about 4 feet. Such a surge will merely flood the beach (up to my knees in the graphic). A category-2 storm is much higher, up to my neck, and probably will flood the beachfront property. The water continues to rise radically with category, with a category-4 storm producing a devastating surge of about 16 feet. A category-5 simply covers the entire beach, with only treetops above the water, and continues inland for great distances destroying just about everything.
Here is an annotated diagram of two images of the SAME BEACH - Naples in Florida. The left image was taken on a typical Florida summer afternoon with light winds and normal conditions. The picture to the right was taken with 50-60 MPH on-shore winds (from the west-northwest) and tides running at least 5 feet above normal. The view in both pictures is to the south and you should be able to see the difference caused by the storm surge. Compare the water level in the right picture to the people standing on the beach to the left. Storm surge is responsible for 90% of hurricane victims due to drowning (The Galveston hurricane of 1900 was such an example where 6,000 people drowned in the surge). Storm surge simply raises the sea level allowing flooding of coastal areas while subjecting beachfront / coastal structures to the destructive power of the wind waves and / or swell that may be superimposed atop the storm surge.
Above is an annotated diagram comprised of three images of Chuck's Seafood restaurant and bar in Fort Pierce, Florida being destroyed by storm surge in hurricane Frances in september 2004. In the leftmost picture, during the beginning of the storm, the dining room area is still intact. The tides are quickly rising and have covered the small beach that extended 20 to 30 feet in front of the dining area (at normal tide levels). Note that the berm (higher area after the beach) is already being eroded. This was the bay, not the ocean, but being near Fort Pierce inlet, tides quickly rushed into the bay with 5-6 foot waves atop the surge.
Above is a diagram of three locations where HURRICANES and TYPHOONS exist. Two of these areas are the NORTH ATLANTIC, EAST PACIFIC (INCLUDING THE CENTRAL PACIFIC), where the name HURRICANE is used. The North Atlantic hurricane season runs from June 1 through November 30 while the Eastern Pacific starts May 15 and also runs to November 30 (the CENTRAL PACIFIC, near Hawaii and west to the date line, is similar, but fewer storms develop there each season). The West Pacific (west of the 180-degree date line) is quite different because there is no "real" season for tropical cyclone activity. Storms can develop anytime of the year, but more so during the northern-hemisphere summer. In this area, the term TYPHOON is used, but otherwise the storm is the same thing as a hurricane. A SUPER TYPHOON denotes a typhoon with winds at or over 145-MPH, and the "SUPER" word is used more in the Pacific (a SUPER HURRICANE is a hurricane with winds at or over 145-MPH, but used rarely).
Above is another diagram of three locations concerning the South Pacific, through Australia, and Indian Ocean. The terminology used is a TROPICAL CYCLONE (or just "CYCLONE") in the same sense as a hurricane or typhoon, where the storm reaches 74-MPH or more. In Australia the term WILLY-WILLY is sometimes used for the CYCLONE strength.
As with anything in nature, "rules" such as tropical cyclone seasons and regions of formation simply DO NOT exist. The above diagram shows two cases of such "odd-ball" occurrances. Tropical storm "Peter" developed in the North Atlantic basin in DECEMBER 2003 in a region climatically impossible for such a storm to develop. The storm was over a warm region of water and missed by hostile upper-level winds that would have disrupted it. Meanwhile - far to its northwest, heavy snow was falling in the northeast Atlantic coast of the United States, after all it was late fall - But "nature" doesn't know that as long as the conditions are right for a tropical cyclone to form!
Tropical cyclones, like any other storm and weather phenomina, can be "chased" and observed. Chasing a hurricane (or typhoon) is, however, a dangerous and logistically challenging activity. There are MANY factors one must understand and consider in order to successfully observe a tropical system, and many of these points are presented in the documentation below.
One of the most exciting and seemingly "daring" excursions with tropical meteorology are carried out by both the US military (Air Force and Navy) and the US Government (Depertment of Commerce - NOAA) where special weather scientists actually fly over, around, and even THROUGH these violent storms to gather more knowledge about them! The US Air Force "53rd Weather Reconaisance Squadron" flies modified WC-130 "Hercules" aircraft into storms, while NOAA's Aircraft Operations Center (the US Department of Commerce) flies two WP-3 "Orion" aircraft as well as a highly modified Gulfstream IV jet into storms. We call these amazing people the "Hurricane Hunters", and their expertise has helped vastly improve forecasting and information about tropical cyclones. The "Hurricane Hunters" literally "chase hurricanes" with an aircraft!
With all this said about just about every aspect on tropical cyclones, this last section covers the MOST IMPORTANT aspect of all - How to protect YOURSELF, your loved ones, and your property! Tropical cyclones are "ocean born" storms, and while many remain out over water and bother no one (maybe except for fish and shipping interests), some do come ashore and pack quite a punch when they do. In addition, hurricane activity is on the INCREASE due to higher water temperatures, and this "increase" is sure making it's mark as of 2004 and 2005. We MUST all be ready, in case the "unthinkable" does (and eventually WILL) happen.
HTML File "schurr.htm" - Developed By Chris Collura
To Return To The HOME Page Of This Site Click The "INDEX.HTM" Link Here!