Information AboutSurfing |
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, December 1981]] Surfing is a Surface Water Sport . The participant is carried along the face of a breaking Wave as it approaches Shore , usually on a Surfboard . In addition to surfboards, surfers make use of Kneeboards , Body Boards (aka Boogie Boards ), Kayak s, Surf Skis , and Their Own Bodies . Surfing-related sports, such as Paddleboarding and Sea Kayaking , do not require waves. Other derivative sports such as Kitesurfing and Windsurfing rely on wind for power. Two major classifications within the sport reflect differences in surfboard design: Longboarding and Shortboard ing. In Tow-in Surfing (often associated with Big Wave Surfing ), the surfer is towed into the wave by a motorized water vehicle, such as a Jetski , because standard paddling is often ineffective when trying to match a large wave's higher speed. GENESIS The first European record of surfing in upon Cooks's death in 1779 . At the time, surfing had already been an integral part of indigenous Hawaiian culture for generations. Native Hawaiian surfers rode waves lying down, sitting or standing on long, hardwood boards. Surfing is a sport of native Hawaiian life as any major sport is part of western life today, if not more. It permeated from Hawaiian society, including religion and myth. Hawaiian chiefs would demonstrate and confirm their authority by the skills they displayed in the surf. HYDRODYNAMICS Swell is generated when wind blows consistently over a large area of open water, called the wind's Fetch . The size of a swell is determined by the strength of the wind, the length of its fetch and its duration. So, surf tends to be larger and more prevalent on coastlines exposed to large expanses of ocean traversed by intense Low Pressure Systems . Local wind conditions affect wave quality, since the ridable surface of a wave can become choppy in blustery conditions. Ideal surf conditions include a light to moderate strength "offshore" wind, since this blows into the front of the wave. The factor which most determines wave shape is the Topography Of The Seabed directly behind and immediately beneath the breaking wave. The contours of the Reef or Sand Bank influence wave shape in two respects. Firstly, the steepness of the incline is proportional to the resulting upthrust. When a swell passes over a sudden steep slope, the force of the upthrust causes the top of the wave to be thrown forward, forming a curtain of water which plunges to the wave trough below. Secondly, the alignment of the contours relative to the swell direction determines the duration of the breaking process. When a swell runs along a slope, it continues to peel for as long as that configuration lasts. When swell wraps into a bay or around an island, the breaking wave gradually diminishes in size, as the wave front becomes stretched by Diffraction . For specific surf spots, the state of the ocean tide can play a significant role in the quality of waves or hazards of surfing there. Tidal variations vary greatly among the various global surfing regions, and the effect the tide has on specific spots can vary greatly among the spots within each area. Locations such as Bali, Panama, and Ireland experience 2-3 meter tide fluctuations, whereas in Hawaii the difference between high and low tide is typically less than one meter. In order to know a surf break one must be sensitive to each of these factors. Each break is different, since the underwater topography of one place is unlike any other. At beach breaks, even the sandbanks change shape from week to week, so it takes commitment to get good waves (a skill dubbed "broceanography" by a few California surfers). That's why surfers have traditionally regarded surfing to be more of a lifestyle than a sport. Of course, you can sometimes be lucky and just turn up when the surf is pumping. But, it is more likely that you will be greeted with the dreaded: "You should have been here yesterday." Nowadays, however, Surf Forecasting is aided by advances in information technology, whereby mathematical modelling graphically depicts the size and direction of swells moving around the globe. The regularity of swell varies across the globe and throughout the year. During winter, heavy swells are generated in the mid-latitudes, when the north and south Polar Front s shift toward the Equator. The predominantly westerly winds generate swells that advance eastward. So, waves tend to be largest on west coasts during the winter months. However, an endless train of Mid-latitude Cyclone s causes the Isobar s to become undulated, redirecting swells at regular intervals toward the tropics. East coasts also receive heavy winter swells when low pressure cells form in the sub-tropics, where their movement is inhibited by slow moving Highs . These lows produce a shorter Fetch than polar fronts, however they can still generate heavy swells, since their slower movement increases the duration of a particular wind direction. After all, the variables of fetch and duration both influence how long the wind acts over a wave as it travels, since a wave reaching the end of a fetch is effectively the same as the wind dying off. During summer, heavy swells are generated when cyclones form in the tropics. Tropical Cyclones form over warm seas, so their occurrence is influenced by El Niño & La Niña cycles. Their movements are unpredictable. They can even move westward, which is unique for a large scale weather system. In 1979, Tropical Cyclone Kerry wandered for 3 weeks across the Coral Sea and into Queensland, before dissipating. The quest for perfect surf has given rise to a field of tourism based on the surfing adventure. Yacht charters and Surf Camps offer surfers access to the high quality surf found in remote, tropical locations, where Tradewinds ensure offshore conditions. Since winter swells are generated by Mid-latitude Cyclone s, their regularity coincides with the passage of these lows. So, the swells arrive in pulses, each lasting for a couple of days, with a couple of days between each swell. Since bigger waves break in a different configuration, a rising swell is yet another variable to consider when assessing how to approach a break. Wave intensity classification of tube shape can be represented as a ratio between length and width. A perfectly cylindrical Classification parameters
Artificial reefs The value of good surf has even prompted the construction of Artificial Reefs and sand bars to attract surf tourism. Of course, there is always the risk that one's holiday coincides with a "flat spell". Wave Pool s aim to solve that problem, by controlling all the elements that go into creating perfect surf, however there are only a handful of wave pools that can simulate good surfing waves, owing primarily to construction and operation costs and potential liability. The availability of free Model Data from the NOAA has allowed the creation of several Surf Forecasting websites. SURFERS AND SURF CULTURE See Also: Surf culture Surfers represent a diverse Culture based on riding the naturally occurring process of ocean waves. Some people practice surfing as a Recreation al activity while others demonstrate extreme devotion to the sport by making it the central focus of their lives. The sport has become so popular that surfing now represents a multi-billion dollar Industry . Some people make a career out of surfing by receiving corporate sponsorships, competing in contests, or marketing and selling surf related products, such as equipment and clothing. Other surfers separate themselves from any and all Commercialism associated with surfing. These soul surfers, as they are often called, practice the sport purely for personal enjoyment and many even find a deeper meaning through involving themselves directly with naturally occurring wave patterns and subscribe to ecological Philosophies , or Ecosophies . On September 2, 2007, in Brazil , 84 Surfers caught the same wave (from Australia, South Africa, Portugal, Britain and the US, to beat the former record of 73 surfers on a wave). But while 300 turned up in Cornwall and Capetown , the Brazilian waxheads won. With only 120 people, surfers in Santos , south-east of Sao Paulo , smashed the South African record.[http://blogs.smh.com.au/sit/archives/2007/09/record_breakers_ready_set_now.html SMH, Record breakers: Ready, set - now pucker up for Bosnia] MANEUVERS Surfing begins with the surfer eyeing a rideable wave on the horizon and then staying ahead of the crest until the surfboard is planing down the wave face, at which point the surfer "pops up." A common problem for beginners is not even being able to catch the wave in the first place, due to faulty positioning and coordination, and conversely, one sign of a good surfer is being able to catch a difficult wave that other surfers cannot, with better positioning and coordination/balance . Once the wave has started to carry the surfer forward, the surfer quickly jumps to his or her feet and proceeds to ride down the face of the wave, sometimes staying just ahead of the breaking part (white water) of the wave (in a place often referred to as "the pocket" or "the curl"), sometimes riding out beyond the pocket toward the shoulder of the wave. This is a difficult process in total, where often everything seems to be happening nearly simultaneously, making it hard for the uninitiated to follow the steps. Surfers' skills are tested not only in their ability to control their board in challenging conditions and/or catch and ride challenging waves, but also by their ability to execute various maneuvers such as turning and carving. Some of the common turns have become recognizable tricks such as the "cutback" (turning back toward the breaking part of the wave), the "floater" (riding on the top of the breaking curl of the wave), and "off the lip" (banking off the top of the wave). A newer addition to surfing has been the progression of the "air" where a surfer is able to propel oneself off the wave and re-enter. Some of these maneuvers are now executed to extreme degrees, as with off-the-lips where a surfer over-rotates his turn and re-enters backward, or airs done in the same fashion, recovering either with re-rotation or continuing the over-rotation to come out with his nose forward again. "Tube riding" is when a surfer maneuvers into a position where the wave curls over the top of him or her, forming a "tube" (or "barrel"), with the rider inside the hollow cylindrical portion of the wave. This difficult and sometimes dangerous procedure is arguably the most coveted and sought after goal in surfing. "Hanging Ten" and "Hanging Five" are moves usually specific to longboarding. Hanging Ten refers to having both feet on the front end of the board with all ten of the surfer's toes off the edge, also known as Noseriding . Hanging Five is having just one foot near the front, and five toes off the edge. Common terms
EQUIPMENT Surfing can be done on various pieces of equipment, including surfboards, bodyboards, wave skis, kneeboards and surf mat. Surfboard s were originally made of solid wood and were generally quite large and heavy (often up to 12 feet long and 100 pounds / 45 kg). Lighter Balsa Wood surfboards (first made in the late 1940s and early 1950s) were a significant improvement, not only in portability, but also in increasing maneuverability on the wave. Most modern surfboards are made of polyurethane foam (with one or more wooden strips or "stringers"), fiberglass cloth, and polyester resin. An emerging surf technology is an epoxy Surfboard , which are stronger and lighter than traditional fiberglass. Even newer surfboard designs incorporate materials such as Carbon Fiber and springy 'firewire'. Equipment used in surfing includes a Leash (to stop a surfer's board from washing to shore after a "wipeout", and to prevent it from hitting other surfers), Surf Wax and/or traction pads (to keep a surfer's feet from slipping off the deck of the board), and "fins" (also known as "skegs") which can either be permanently attached ("glassed-on") or interchangeable. In warmer climates swimsuits, surf trunks or Boardshorts are worn, and occasionally Rash Guard s; in cold water surfers can opt to wear Wetsuit s, boots, hoods, and gloves to protect them against lower water temperatures. There are many different Surfboard sizes, shapes, and designs in use today. Modern Longboard s, generally 9 to 10 feet in length, are reminiscent of the earliest surfboards, but now benefit from all the modern innovations of surfboard shaping and fin design. The modern Shortboard began its life in the late 1960s evolving up to today's common "thruster" style shortboard, a three fin design, usually around 6 to 7 feet in length. |
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