Waterspout

Climatology Though the majority of waterspouts occur in the tropics, they can seasonally appear in temperate areas throughout the world, and are common across the western coast of Europe as well as the British Isles and several areas of the Mediterranean and Baltic Sea. They are not restricted to saltwater; many have been reported on lakes and rivers including the Great Lakes and the St. Lawrence River. They are fairly common on the Great Lakes during late summer and early fall, with a record 66+ waterspouts reported over just a seven-day period in 2003. Waterspouts are also frequently observed off the east coast of Australia, with several being described by Joseph Banks during the voyage of the Endeavour in 1770. File:Great Lakes Waterspouts.jpg|A family of four waterspouts seen on Lake Huron, 9 September 1999 File:Quadruple Waterspout Summerland Key June 5, 2009.jpg|Four waterspouts seen in the Florida Keys, 5 June 2009 File:CSIRO ScienceImage 7790 A waterspout over the Tasman Sea.jpg|Waterspout in the Tasman Sea, 29 January 2009 File:Waterspout 3 (14276517300).jpg|Waterspout in Adelaide, South Australia, June 20, 2014. Formation Waterspouts exist on a microscale, where their environment is less than two kilometers in width. The cloud from which they develop can be as innocuous as a moderate cumulus, or as great as a supercell. While some waterspouts are strong and tornadic in nature, most are much weaker and caused by different atmospheric dynamics. They normally develop in moisture-laden environments as their parent clouds are in the process of development, and it is theorized they spin as they move up the surface boundary from the horizontal shear near the surface, and then stretch upwards to the cloud once the low-level shear vortex aligns with a developing cumulus cloud or thunderstorm. Some weak tornadoes, known as landspouts, have been shown to develop in a similar manner. More than one waterspout can occur simultaneously in the same vicinity. In 2012, as many as nine simultaneous waterspouts were reported on Lake Michigan in the United States. ==Types==

Non-tornadic in the Netherlands, 27 August 2006 Waterspouts that are not associated with a rotating updraft of a supercell thunderstorm are known as "non-tornadic" or "fair-weather" waterspouts. By far the most common type of waterspout, these occur in coastal waters and are associated with dark, flat-bottomed, developing convective cumulus towers. Fair-weather waterspouts develop and dissipate rapidly, having life cycles shorter than 20 minutes. They are most frequently seen in tropical and sub-tropical climates, with upwards of 400 per year observed in the Florida Keys. Tornadic , caused by a severe thunderstorm, 15 July 2005 "Tornadic waterspouts", also accurately referred to as "tornadoes over water", are formed from mesocyclones in a manner essentially identical to land-based tornadoes in connection with severe thunderstorms, but simply occurring over water. A tornado which travels from land to a body of water would also be considered a tornadic waterspout. Since the vast majority of mesocyclonic thunderstorms in the United States occur in land-locked areas, true tornadic waterspouts are correspondingly rarer than their fair-weather counterparts in that country. However, in some areas, such as the Adriatic, Aegean and Ionian Seas, tornadic waterspouts can make up half of the total number. Snowspout A winter waterspout, also known as an icespout, an ice devil, or a snowspout, is a rare instance of a waterspout forming under the base of a snow squall. The term "winter waterspout" is used to differentiate between the common warm season waterspout and this rare winter season event. There are a couple of critical criteria for the formation of a winter waterspout. Very cold temperatures need to be present over a body of water, which is itself warm enough to produce fog resembling steam above the water's surface. Like the more efficient lake-effect snow events, winds focusing down the axis of long lakes enhance wind convergence and increase the likelihood of a winter waterspout developing. The terms "snow devil" and "snownado" describe a different phenomenon: a snow vortex close to the surface with no parent cloud, similar to a dust devil. ==Impacts==

Human , Wales, by a Royal Air Force Search and Rescue crew, 15 November 2010 Waterspouts have long been recognized as serious marine hazards. Stronger waterspouts pose a threat to watercraft, aircraft and people. It is recommended to keep a considerable distance from these phenomena, and to always be on alert through weather reports. The United States National Weather Service will often issue special marine warnings when waterspouts are likely or have been sighted over coastal waters, or tornado warnings when waterspouts are expected to move onshore. Incidents of waterspouts causing severe damage and casualties are rare; however, there have been several notable examples. The Malta tornado of 1551 was the earliest recorded occurrence of a deadly waterspout. It struck the Grand Harbour of Valletta, sinking four galleys and numerous boats, and killing hundreds of people. The 1851 Sicily tornadoes were twin waterspouts that made landfall in western Sicily, ravaging the coast and countryside before ultimately dissipating back again over the sea. In August 2024, a waterspout has been reported by some witnesses of the sinking of the large yacht Bayesian off the coast of Sicily and might have been the cause or an aggravating circumstance. Of the 22 people on the boat, seven died and 15 were rescued. Natural Depending on how fast the winds from a waterspout are whipping, anything that is within about of the surface of the water, including fish of different sizes, frogs, and even turtles, can be lifted into the air. A waterspout can sometimes suck small animals such as fish out of the water and all the way up into the cloud. Even if the waterspout stops spinning, the fish in the cloud can be carried over land, buffeted up and down and around with the cloud's winds until its currents no longer keep the fish airborne. Depending on how far they travel and how high they are taken into the atmosphere, the fish are sometimes dead by the time they rain down. People as far as inland have experienced raining fish. Fish can also be sucked up from rivers, but raining fish is not a common weather phenomenon. == Research and forecasting ==

The Szilagyi Waterspout Index (SWI), developed by Canadian meteorologist Wade Szilagyi, is used to predict conditions favorable for waterspout development. The SWI ranges from −10 to +10, where values greater than or equal to zero represent conditions favorable for waterspout development. The International Centre for Waterspout Research (ICWR) is a non-governmental organization of individuals from around the world who are interested in the field of waterspouts from a research, operational and safety perspective. Originally a forum for researchers and meteorologists, the ICWR has expanded interest and contribution from storm chasers, the media, the marine and aviation communities and from private individuals. == Myths ==

'' by William Hodges, 1776 There was a commonly held belief among sailors in the 18th and 19th centuries that shooting a broadside cannon volley dispersed waterspouts. Among others, Captain Vladimir Bronevskiy claims that it was a successful technique, having been an eyewitness to the dissipation of a phenomenon in the Adriatic while a midshipman aboard the frigate Venus during the 1806 campaign under Admiral Senyavin. A waterspout has been proposed as a reason for the abandonment of the Mary Celeste. ==See also==