In meteorology, a cyclone is an area of closed, circular fluid motion rotating in the same direction as the Earth. This is usually characterized by inward spiraling winds that rotate counter clockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere of the Earth. Most large-scale cyclonic circulations are centered on areas of low atmospheric pressure. The largest low-pressure systems are cold-core polar cyclones and extratropical cyclones which lie on the synoptic scale. Warm-core cyclones such as tropical cyclones, mesocyclones, and polar lows lie within the smaller mesoscale. Subtropical cyclones are of intermediate size. Upper level cyclones can exist without the presence of a surface low, and can pinch off from the base of the Tropical Upper Tropospheric Trough during the summer months in the Northern Hemisphere. Cyclones have also been seen on extraterrestrial planets, such as Mars and Neptune.

Cyclogenesis describes the process of cyclone formation and intensification. Extratropical cyclones form as waves in large regions of enhanced mid-latitude temperature contrasts called baroclinic zones. These zones contract to form weather fronts as the cyclonic circulation closes and intensifies. Later in their life cycle, cyclones occlude as cold core systems. A cyclone's track is guided over the course of its 2 to 6 day life cycle by the steering flow of the cancer or subtropical jet stream.

Weather fronts separate two masses of air of different densities and are associated with the most prominent meteorological phenomena. Air masses separated by a front may differ in temperature or humidity. Strong cold fronts typically feature narrow bands of thunderstorms and severe weather, and may on occasion be preceded by squall lines or dry lines. They form west of the circulation center and generally move from west to east. Warm fronts form east of the cyclone center and are usually preceded by stratiform precipitation and fog. They move poleward ahead of the cyclone path. Occluded fronts form late in the cyclone life cycle near the center of the cyclone and often wrap around the storm center.

Tropical cyclogenesis describes the process of development of tropical cyclones. Tropical cyclones form due to latent heat driven by significant thunderstorm activity, and are warm core. Cyclones can transition between extratropical, subtropical, and tropical phases under the right conditions. Mesocyclones form as warm core cyclones over land, and can lead to tornado formation. Waterspouts can also form from mesocyclones, but more often develop from environments of high instability and low vertical wind shear.

Structure

There are a number of structural characteristics common to all cyclones. As they are low pressure areas, their center is the area of lowest atmospheric pressure in the region, often known in mature tropical cyclones as the eye. Near the center, the pressure gradient force (from the pressure in the center of the cyclone compared to the pressure outside the cyclone) and the Coriolis force must be in an approximate balance, or the cyclone would collapse on itself as a result of the difference in pressure. The wind flow around a large cyclone is counterclockwise in the northern hemisphere and clockwise in the southern hemisphere as a result of the Coriolis effect. (An anticyclone, on the other hand, rotates clockwise in the northern hemisphere, and counterclockwise in the southern hemisphere.)

Formation

Cyclogenesis is the development or strengthening of cyclonic circulation in the atmosphere (a low pressure area). Cyclogenesis is an umbrella term for several different processes, all of which result in the development of some sort of cyclone. It can occur at various scales, from the microscale to the synoptic scale. Extratropical cyclones form as waves along weather fronts before occluding later in their life cycle as cold core cyclones. Tropical cyclones form due to latent heat driven by significant thunderstorm activity, and are warm core. Mesocyclones form as warm core cyclones over land, and can lead to tornado formation. Waterspouts can also form from mesocyclones, but more often develop from environments of high instability and low vertical wind shear. Cyclogenesis is the opposite of cyclolysis, and has an anticyclonic (high pressure system) equivalent which deals with the formation of high pressure areas—Anticyclogenesis.

The surface low has a variety of ways of forming. Topography can force a surface low when dense low-level high pressure system ridges in east of a north-south mountain barrier. Mesoscale convective systems can spawn surface lows which are initially warm core. The disturbance can grow into a wave-like formation along the front and the low will be positioned at the crest. Around the low, flow will become cyclonic, by definition. This rotational flow will push polar air equatorward west of the low via its trailing cold front, and warmer air with push poleward low via the warm front. Usually the cold front will move at a quicker pace than the warm front and “catch up” with it due to the slow erosion of higher density airmass located out ahead of the cyclone and the higher density airmass sweeping in behind the cyclone, usually resulting in a narrowing warm sector. At this point an occluded front forms where the warm air mass is pushed upwards into a trough of warm air aloft, which is also known as a trowal.

Tropical cyclogenesis is the technical term describing the development and strengthening of a tropical cyclone in the atmosphere. The mechanisms through which tropical cyclogenesis occurs are distinctly different from those through which mid-latitude cyclogenesis occurs. Tropical cyclogenesis involves the development of a warm-core cyclone, due to significant convection in a favorable atmospheric environment. There are six main requirements for tropical cyclogenesis: sufficiently warm sea surface temperatures, atmospheric instability, high humidity in the lower to middle levels of the troposphere, enough Coriolis force to develop a low pressure center, a preexisting low level focus or disturbance, and low vertical wind shear. An average of 86 tropical cyclones of tropical storm intensity form annually worldwide, with 47 reaching hurricane/typhoon strength, and 20 becoming intense tropical cyclones (at least Category 3 intensity on the Saffir-Simpson Hurricane Scale).

Surface-based types

There are six main types of cyclones: Polar cyclones, Polar lows, Extratropical cyclones, Subtropical cyclones, Tropical cyclones, and Mesocyclones

Polar cyclone

A polar, sub-polar, or Arctic cyclone (also known as a polar vortex) is a vast area of low pressure which strengthens in the winter and weakens in the summer. A polar cyclone is a low pressure weather system, usually spanning to , in which the air circulates in a counterclockwise direction in the northern hemisphere, and a clockwise direction in the southern hemisphere. In the Northern Hemisphere, the polar cyclone has two centers on average. One center lies near Baffin Island and the other over northeast Siberia. In the southern hemisphere, it tends to be located near the edge of the Ross ice shelf near 160 west longitude. When the polar vortex is strong, westerly flow descends to the Earth's surface. When the polar cyclone is weak, significant cold outbreaks occur.

Polar low

A polar low is a small-scale, short-lived atmospheric low pressure system (depression) that is found over the ocean areas poleward of the main polar front in both the Northern and Southern Hemispheres. During winter, when cold-core lows with temperatures in the mid-levels of the troposphere reach move over open waters, deep convection forms which allows polar low development to become possible. The systems usually have a horizontal length scale of less than and exist for no more than a couple of days. They are part of the larger class of mesoscale weather systems. Polar lows can be difficult to detect using conventional weather reports and are a hazard to high-latitude operations, such as shipping and gas and oil platforms. Polar lows have been referred to by many other terms, such as polar mesoscale vortex, Arctic hurricane, Arctic low, and cold air depression. Today the term is usually reserved for the more vigorous systems that have near-surface winds of at least 17 m/s.

Extratropical

An extratropical cyclone is a synoptic scale low pressure weather system that has neither tropical nor polar characteristics, being connected with fronts and horizontal gradients in temperature and dew point otherwise known as "baroclinic zones".

The descriptor "extratropical" refers to the fact that this type of cyclone generally occurs outside of the tropics, in the middle latitudes of the planet. These systems may also be described as "mid-latitude cyclones" due to their area of formation, or "post-tropical cyclones" where extratropical transition has occurred, and are often described as "depressions" or "lows" by weather forecasters and the general public. These are the everyday phenomena which along with anti-cyclones, drive the weather over much of the Earth.

Although extratropical cyclones are almost always classified as baroclinic since they form along zones of temperature and dewpoint gradient within the westerlies, they can sometimes become barotropic late in their life cycle when the temperature distribution around the cyclone becomes fairly uniform with radius. An extratropical cyclone can transform into a subtropical storm, and from there into a tropical cyclone, if it dwells over warm waters and develops central convection, which warms its core.

Subtropical

A subtropical cyclone is a weather system that has some characteristics of a tropical cyclone and some characteristics of an extratropical cyclone. They can form between the equator and the 50th parallel. As early as the 1950s, meteorologists were unclear whether they should be characterized as tropical cyclones or extratropical cyclones, and used terms such as quasi-tropical and semi-tropical to describe the cyclone hybrids. By 1972, the National Hurricane Center officially recognized this cyclone category. Subtropical cyclones began to receive names off the official tropical cyclone list in the Atlantic Basin in 2002. They have broad wind patterns with maximum sustained winds located farther from the center than typical tropical cyclones, and exist in areas of weak to moderate temperature gradient.

Since they form from initially extratropical cyclones which have colder temperatures aloft than normally found in the tropics, the sea surface temperatures required for their formation are lower than the tropical cyclone threshold by three degrees Celsius, or five degrees Fahrenheit, lying around 23 degrees Celsius. This means that subtropical cyclones are more likely to form outside the traditional bounds of the hurricane season. Although subtropical storms rarely have hurricane-force winds, they may become tropical in nature as their cores warm.

Tropical

A tropical cyclone is a storm system characterized by a low pressure center and numerous thunderstorms that produce strong winds and flooding rain. A tropical cyclone feeds on heat released when moist air rises, resulting in condensation of water vapour contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as nor'easters, European windstorms, and polar lows, leading to their classification as "warm core" storm systems.

The term "tropical" refers to both the geographic origin of these systems, which form almost exclusively in tropical regions of the globe, and their formation in Maritime Tropical air masses. The term "cyclone" refers to such storms' cyclonic nature, with counterclockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere. Depending on their location and strength, tropical cyclones are referred to by other names, such as hurricane, typhoon, tropical storm, cyclonic storm, tropical depression, or simply as a cyclone. A tropical cyclone is generally referred to as a hurricane (from the name of the ancient Central American deity of wind, Huracan) in the Atlantic basin, and a cyclone in the Indian Ocean and parts of the Pacific.

While tropical cyclones can produce extremely powerful winds and torrential rain, they are also able to produce high waves and damaging storm surge. They develop over large bodies of warm water, and lose their strength if they move over land. This is the reason coastal regions can receive significant damage from a tropical cyclone, while inland regions are relatively safe from receiving strong winds. Heavy rains, however, can produce significant flooding inland, and storm surges can produce extensive coastal flooding up to from the coastline. Although their effects on human populations can be devastating, tropical cyclones can also relieve drought conditions. They also carry heat and energy away from the tropics and transport it toward temperate latitudes, which makes them an important part of the global atmospheric circulation mechanism. As a result, tropical cyclones help to maintain equilibrium in the Earth's troposphere.

Many tropical cyclones develop when the atmospheric conditions around a weak disturbance in the atmosphere are favorable. Others form when other types of cyclones acquire tropical characteristics. Tropical systems are then moved by steering winds in the troposphere; if the conditions remain favorable, the tropical disturbance intensifies, and can even develop an eye. On the other end of the spectrum, if the conditions around the system deteriorate or the tropical cyclone makes landfall, the system weakens and eventually dissipates. A tropical cyclone can become extratropical as it moves toward higher latitudes if its energy source changes from heat released by condensation to differences in temperature between air masses; From an operational standpoint, a tropical cyclone is usually not considered to become subtropical during its extratropical transition.

Mesocyclone

A mesocyclone is a vortex of air, to in diameter (the mesoscale of meteorology), within a convective storm. Air rises and rotates around a vertical axis, usually in the same direction as low pressure systems in both northern and southern hemisphere. They are most often cyclonic, that is, associated with a localized low-pressure region within a supercell. Such storms can feature strong surface winds and severe hail. Mesocyclones often occur together with updrafts in supercells, where tornadoes may form. About 1700 mesocyclones form annually across the United States, but only half produce tornadoes.

Cyclones are not unique to Earth. Cyclonic storms are common on Jovian planets, like the Small Dark Spot on Neptune. Also known as the Wizard's Eye, it is about one third the diameter of the Great Dark Spot. It received the name "Wizard's Eye" because it looks like an eye. This appearance is caused by a white cloud in the middle of the Wizard's Eye. Mars has also exhibited cyclonic storms. Jovian storms like the Great Red Spot are usually mistakenly named as giant hurricanes or cyclonic storms. However, this is inaccurate, as the Great Red Spot is, in fact, the inverse phenomenon, an anticyclone.

TUTT cell

Under specific circumstances, upper cold lows can break off from the base of the Tropical Upper Tropospheric Trough (TUTT), which is located mid-ocean in the Northern Hemisphere during the summer months. These upper tropospheric cyclonic vortices, also known as TUTT cells or TUTT lows, usually move slowly from east-northeast to west-southwest, and generally do not extend below 20,000 feet in altitude. A weak inverted surface trough within the trade wind is generally found underneath them, and they may also be associated with broad areas of high-level clouds. Downward development results in an increase of cumulus clouds and the appearance of a surface vortex. In rare cases, they become warm-core, resulting in the vortex becoming a tropical cyclone. Upper cyclones and upper troughs which trail tropical cyclones can cause additional outflow channels and aid in their intensification process. Developing tropical disturbances can help create or deepen upper troughs or upper lows in their wake due to the outflow jet emanating from the developing tropical disturbance/cyclone.

References

External links

Fundamental of Physical Geography: The Mid-Latitude Cyclone – Dr. Michael Pidwirny, University of British Columbia, Okanagan

Glossary Definition: Cyclogenesis – The National Snow and Ice Data Center

Glossary Definition: Cyclolysis – The National Snow and Ice Data Center

Weather Facts: The Polar Low – Weather Online UK

NOAA FAQ

Cyclones 'ClearlyExplained'

Cyclone Video Archive

The EM-DAT International Disaster Database by the Centre for Research on the Epidemiology of Disasters

cyclone rita

Category:Basic meteorological concepts and phenomena Category:Tropical cyclone meteorology * Category:Weather hazards Category:Vortices

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name	Baby Bash
background	solo_singer
birth name	Ronnie Ray Bryant
born	Vallejo, California
origin	Houston, Texas, United States
instrument	Vocals
genre	Latino, Hip Hop, Pop Rap, R&B;
occupation	Singer, Songwriter, Actor, Performer
Years active	1996-present (singing) 2002-present (acting)
label	Dope House, Universal, RCA, J, Arista, Bashtown Music Group
associated acts	Frankie J, South Park Mexican, Akon, Lucky Luciano, T-Pain
website	}}

Ronnie Rey Bryant (born 1975), better known by his stage name Baby Bash (formerly Baby Beesh), is a Mexican-American rapper. From 1995 to 1998, he performed under the stage name ''Baby Beesh'', as part of the Vallejo, California group Potna Duece, after which he changed the last part of the name to ''Bash''. His first album was "On Tha Cool", with one of his greatest hits, "Vamanos"... His next album "The Smokin' Nephew" which included the singles "Suga Suga" and "Shorty Doowop". In 2005, ''Super Saucy'' was released, its lead single being "Baby I'm Back", a collaboration with singer Akon. ''Cyclone'' followed in 2007, with its title single featuring T-Pain and its follow-up, "What Is It" featuring Sean Kingston, landing on the ''Billboard'' charts as well.

He has frequently contributed to other performers' works, including a spot in the song "Obsession (No Es Amor)" by 3rd Wish released in Europe and later a U.S release with a copy / re- recording of the European version, performed by Frankie J in 2005 and "Doing Too Much" by Paula DeAnda in 2006.

Early life

Ronnie Rey Bryant was born to a Mexican American mother and English American father; Bryant's father became a heroin and crack cocaine addict. Bryant was raised by his grandmother, and Bryant's uncles exposed him to many different types of musical genres. Initially, Bryant wanted to be a professional basketball player. He planned to play basketball for the junior college he attended in California during the mid-'90s. After tearing his ankle several times and not having it repaired with surgery, he permanently ended the possibility of ever playing basketball at even a semi-professional level.

Career

Baby Bash's career began as part of the group Potna Duece in Vallejo, California. He went to Houston in 2000, where he met fellow rapper South Park Mexican. Prior to his success as a solo artist he, under the name "Baby Beesh", was part of rap groups Potna Deuce and Latino Velvet. Bash's debut album entitled ''Savage Dreams'' was released on the independent label Dope House Records in 2001. The acclaim he received soon caught the attention of Universal Records, who signed him later that year. In 2003, Baby Bash released his first album on a major label, ''Tha Smokin' Nephew'', and ''Super Saucy'' in 2005. He recently was featured in Paula DeAnda's first single "Doin' Too Much" from her debut album ''Paula DeAnda''. He has collaborated with numerous other artists during his career, such as West Coast rappers B-Legit, C-Bo, Coolio- Da'unda'dogg, E-40 and Mac Dre, R&B; singers like Akon, Avant, Natalie, Mario, and Nate Dogg, and other Latino rappers such as Fat Joe, Nino Brown, Doll-E Girl, Frost, and Pitbull. He continues to write lyrics for singers such as Paula DeAnda, Whitney Houston, Jennifer Hudson and Frankie J.

His third studio album, ''Cyclone'' (initially titled ''Ronnie Rey All Day''), was released in late October 2007. So far, Baby Bash has released three singles off the album: "Mamacita" featuring Marcos Hernandez, "Na Na (The Yummy Song)", and "Cyclone" featuring Mickaël & T-Pain. The month of the album release, Baby Bash became Myspace's #1 Latin artist, and the single Cyclone had over 750,000 digital and ringtone sales prior to the album's release.

Baby Bash completed a film entitled ''Primos'' starring Chingo Bling and Danny Trejo. The comedy involves three cousins working in a bakery with dreams of making money, and is slated for a 2010 release. His major-label debut ''Tha Smokin' Nephew'' was well-received by Allmusic, but his 2007 album ''Cyclone'' was given mixed reviews, for example being panned by ''Rolling Stone'' magazine.

In December 2010, Baby Bash was offered a job as on-air personality for Wild 94.9, a Rhythmic Contemporary commercial radio station in San Francisco, California. In the same month, it was announced that Bash was endorsing a new energy drink for women named after his 2011 album's single, "Go Girl." Part of the sales proceeds from the energy drink will be donated to various charities for breast cancer and ovarian cancer research for women. His latest album ''Bashtown'' was released on March 22, 2011, and features guest appearances by Lloyd and E-40.

Discography

2001: ''Savage Dreams''

2002: ''On tha Cool''

2003: ''Tha Smokin' Nephew''

2004: ''Menage a Trois''

2005: ''Super Saucy''

2007: ''Cyclone''

2011: ''Bashtown

2012: ''Weedsmoke

References

External links

Category:1975 births Category:Date of birth missing (living people) Category:Living people Category:American musicians of English descent Category:American rappers of Mexican descent Category:Electro-hop musicians Category:Hip hop singers Category:People from Vallejo, California Category:Rappers from Houston, Texas Category:Rappers from the San Francisco Bay Area Category:RCA Records artists Category:Universal Records artists Category:Hispanic and Latino American rappers Category:Hispanic and Latino American people

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