Large hailstone with concentric rings

Hail is a form of solid precipitation. It consists of balls or irregular lumps of ice, each of which is referred to as a hail stone. Unlike graupel, which is made of rime, and ice pellets, which are smaller and translucent, hail stones – on Earth – consist mostly of water ice and measure between 5 and 200 millimetres (0.20 and 7.9 in) in diameter.^{[citation needed]} The METAR reporting code for hail 5 mm (0.20 in) or greater is GR, while smaller hailstones and graupel are coded GS. Hail is possible within most thunderstorms as it is produced by cumulonimbi (thunderclouds),^[1] and within 2 nautical miles (3.7 km) of the parent storm. Hail formation requires environments of strong, upward motion of air with the parent thunderstorm (similar to tornadoes) and lowered heights of the freezing level. In the mid-latitudes, hail forms near the interiors of continents, while in the tropics, it tends to be confined to high elevations.

There are methods available to detect hail-producing thunderstorms using weather satellites and weather radar imagery. Hail stones generally fall at higher speeds as they grow in size, though complicating factors such as melting, friction with air, wind, and interaction with rain and other hail stones can slow their descent through Earth's atmosphere. Severe weather warnings are issued for hail when the stones reach a damaging size, as it can cause serious damage to human-made structures and, most commonly, farmers' crops.

Definition[link]

A large hailstone, about 6 cm (2.36 in) in diameter

Any thunderstorm which produces hail that reaches the ground is known as a hailstorm.^[2] Hail has a diameter of 5 millimetres (0.20 in) or more.^[1] Hail stones can grow to 15 centimetres (6 in) and weigh more than 0.5 kilograms (1.1 lb).^[3]

Unlike ice pellets, hail stones are layered and can be irregular and clumped together. Hail is composed of transparent ice or alternating layers of transparent and translucent ice at least 1 millimetre (0.039 in) thick, which are deposited upon the hail stone as it cycles through the cloud, suspended aloft by air with strong upward motion until its weight overcomes the updraft and falls to the ground. Although the diameter of hail is varied, in the United States, the average observation of damaging hail is between 2.5 cm (1 in) and golf ball-sized (1.75 in).^[4]

Stones larger than 2 cm (0.75 in) are usually considered large enough to cause damage. The Meteorological Service of Canada will issue severe thunderstorm warnings when hail that size or above is expected.^[5] The US National Weather Service has a 2.5 cm (1 in) or greater in diameter threshold, effective January 2010, an increase over the previous threshold of ¾-inch hail.^[6] Other countries will have different thresholds according local sensitivity to hail; for instance grape growing areas could be adversely impacted by smaller hailstones. Hailstones can be very large or very small, depending on how strong the updraft is: weaker hailstorms produce smaller hailstones than stronger hailstorms (such as supercells).

Formation[link]

Hail forms in strong thunderstorm clouds, particularly those with intense updrafts, high liquid water content, great vertical extent, large water droplets, and where a good portion of the cloud layer is below freezing 0 °C (32 °F).^[1] These types of strong updrafts can also indicate the presence of a tornado.^[7] The growth rate is maximized where air is near a temperature of −13 °C (9 °F).

Layer nature of the hailstones[link]

Hail shaft

Severe thunderstorms containing hail can exhibit a characteristic green coloration^[8]

Like other precipitation in cumulonimbus clouds hail begins as water droplets. As the droplets rise and the temperature goes below freezing, they become supercooled water and will freeze on contact with condensation nuclei. A cross-section through a large hailstone shows an onion-like structure. This means the hailstone is made of thick and translucent layers, alternating with layers that are thin, white and opaque. Former theory suggested that hailstones were subjected to multiple descents and ascents, falling into a zone of humidity and refreezing as they were uplifted. This up and down motion was thought to be responsible for the successive layers of the hailstone. New research (based on theory and field study) has shown this is not necessarily true.

The storm's updraft, with upwardly directed wind speeds as high as 110 miles per hour (180 km/h),^[9] blow the forming hailstones up the cloud. As the hailstone ascends it passes into areas of the cloud where the concentration of humidity and supercooled water droplets varies. The hailstone’s growth rate changes depending on the variation in humidity and supercooled water droplets that it encounters. The accretion rate of these water droplets is another factor in the hailstone’s growth. When the hailstone moves into an area with a high concentration of water droplets, it captures the latter and acquires a translucent layer. Should the hailstone move into an area where mostly water vapour is available, it acquires a layer of opaque white ice.^[10]

Furthermore, the hailstone’s speed depends on its position in the cloud’s updraft and its mass. This determines the varying thicknesses of the layers of the hailstone. The accretion rate of supercooled water droplets onto the hailstone depends on the relative velocities between these water droplets and the hailstone itself. This means that generally the larger hailstones will form some distance from the stronger updraft where they can pass more time growing.^[10] As the hailstone grows it releases latent heat, which keeps its exterior in a liquid phase. Undergoing 'wet growth', the outer layer is sticky, or more adhesive, so a single hailstone may grow by collision with other smaller hailstones, forming a larger entity with an irregular shape.^[11]

The hailstone will keep rising in the thunderstorm until its mass can no longer be supported by the updraft. This may take at least 30 minutes based on the force of the updrafts in the hail-producing thunderstorm, whose top is usually greater than 10 km high. It then falls toward the ground while continuing to grow, based on the same processes, until it leaves the cloud. It will later begin to melt as it passes into air above freezing temperature.^[12]

Thus, a unique trajectory in the thunderstorm is sufficient to explain the layer-like structure of the hailstone. The only case in which we can discuss multiple trajectories is in a multicellular thunderstorm where the hailstone may be ejected from the top of the "mother" cell and captured in the updraft of a more intense "daughter cell". This however is an exceptional case.^[10]

Factors favoring hail[link]

Hail is most common within continental interiors of the mid-latitudes, as hail formation is considerably more likely when the freezing level is below the altitude of 11,000 feet (3,400 m).^[13] Movement of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in. Accordingly, hail is actually less common in the tropics despite a much higher frequency of thunderstorms than in the mid-latitudes because the atmosphere over the tropics tends to be warmer over a much greater depth. Hail in the tropics occurs mainly at higher elevations.^[14]

Hail growth becomes vanishingly small when air temperatures fall below −30 °C (−22 °F) as supercooled water droplets become rare at these temperatures.^[13] Around thunderstorms, hail is most likely within the cloud at elevations above 20,000 feet (6,100 m). Between 10,000 feet (3,000 m) and 20,000 feet (6,100 m), 60 percent of hail is still within the thunderstorm, though 40 percent now lies within the clear air under the anvil. Below 10,000 feet (3,000 m), hail is equally distributed in and around a thunderstorm to a distance of 2 nautical miles (3.7 km).^[15]

Climatology[link]

Hail occurs most frequently within continental interiors at mid-latitudes and is less common in the tropics, despite a much higher frequency of thunderstorms than in the midlatitudes.^[16] Hail is also much more common along mountain ranges because mountains force horizontal winds upwards (known as orographic lifting), thereby intensifying the updrafts within thunderstorms and making hail more likely.^[17] One of the more common regions for large hail is across mountainous northern India, which reported one of the highest hail-related death tolls on record in 1888.^[18] China also experiences significant hailstorms.^[19] Central Europe and southern Australia also experience a lot of hailstorms. Popular regions for hailstorms are southern and western Germany, northern and eastern France and southern and eastern Benelux. In south-eastern Europe, Croatia and Serbia experience frequent occurrences of hail.^[20]

In North America, hail is most common in the area where Colorado, Nebraska, and Wyoming meet, known as "Hail Alley."^[21] Hail in this region occurs between the months of March and October during the afternoon and evening hours, with the bulk of the occurrences from May through September. Cheyenne, Wyoming is North America's most hail-prone city with an average of nine to ten hailstorms per season.^[22]

Short-term detection[link]

Example of a three body spike: the weak triangular echoes (pointed by the arrow) behind the red and white thunderstorm core are related to hail inside the storm.

Weather radar is a very useful tool to detect the presence of hail-producing thunderstorms. However, radar data has to be complemented by a knowledge of current atmospheric conditions which can allow one to determine if the current atmosphere is conducive to hail development.

Modern radar scans many angles around the site. Reflectivity values at multiple angles above ground level in a storm are proportional to the precipitation rate at those levels. Summing reflectivities in the Vertically Integrated Liquid or VIL, gives the liquid water content in the cloud. Research shows that hail development in the upper levels of the storm is related to the evolution of VIL. VIL divided by the vertical extent of the storm, called VIL density, has a relationship with hail size, although this varies with atmospheric conditions and therefore is not highly accurate.^[23] Traditionally, hail size and probability can be estimated from radar data by computer using algorithms based on this research. Some algorithms include the height of the freezing level to estimate the melting of the hailstone and what would be left on the ground.

Certain patterns of reflectivity are important clues for the meteorologist as well. The three body scatter spike is an example. This is the result of energy from the radar hitting hail and being deflected to the ground, where they deflect back to the hail and then to the radar. The energy took more time to go from the hail to the ground and back, as opposed to the energy that went direct from the hail to the radar, and the echo is further away from the radar than the actual location of the hail on the same radial path, forming a cone of weaker reflectivities.

More recently, the polarization properties of weather radar returns have been analyzed to differentiate between hail and heavy rain.^[24][25] The use of differential reflectivity (Failed to parse (Missing texvc executable; please see math/README to configure.): Z_{dr} ), in combination with horizontal reflectivity (Failed to parse (Missing texvc executable; please see math/README to configure.): Z_{h} ) has led to a variety of hail classification algorithms.^[26] Visible satellite imagery is beginning to be used to detect hail, but false alarm rates remain high using this method.^[27]

Size and terminal velocity[link]

The size of hail stones is best determined by measuring their diameter with a ruler. In the absence of a ruler, hail stone size is often visually estimated by comparing its size to that of known objects, such as coins.^[28] Below is a table of commonly used objects for this purpose.^[29] Note that using the objects such as hen's eggs, peas, and marbles for comparing hailstone sizes is often inaccurate, due to their varied dimensions. The UK organisation, TORRO, also scales for both hailstones and hailstorms.^[30] When observed at an airport, METAR code is used within a surface weather observation which relates to the size of the hail stone. Within METAR code, GR is used to indicate larger hail, of a diameter of at least 0.25 inches (6.4 mm). GR is derived from the French word grêle. Smaller-sized hail, as well as snow pellets, use the coding of GS, which is short for the French word grésil.^[31]

Terminal velocity of hail, or the speed at which hail is falling when it strikes the ground, varies by the diameter of the hail stones. A hail stone of 1 centimetre (0.39 in) in diameter falls at a rate of 9 metres per second (20 mph), while stones the size of 8 centimetres (3.1 in) in diameter fall at a rate of 48 metres per second (110 mph). Hail stone velocity is dependent on the size of the stone, friction with air it is falling through, the motion of wind it is falling through, collisions with raindrops or other hail stones, and melting as the stones fall through a warmer atmosphere.^[32]

Hailstones ranging in size from Pea to Nickel

A large hailstone, approximately 13.3 cm (5 1/4 inches) in diameter, that fell in Harper, Kansas on May 14, 2004.

Hazards[link]

The largest recorded hailstone in the United States by diameter 8 inches (20 cm) and weight 1.93 pounds (0.88 kg). The hailstone fell in Vivian, South Dakota on July 23, 2010.

Hailstorm in Bogotá, Colombia.

Hail can cause serious damage, notably to automobiles, aircraft, skylights, glass-roofed structures, livestock, and most commonly, farmers' crops.^[22] Hail damage to roofs often goes unnoticed until further structural damage is seen, such as leaks or cracks. It is hardest to recognize hail damage on shingled roofs and flat roofs, but all roofs have their own hail damage detection problems.^[35] Metal roofs are fairly resistant to hail damage, but may accumulate cosmetic damage in the form of dents and damaged coatings.^[36]

Hail is one of the most significant thunderstorm hazards to aircraft.^[37] When hail stones exceed 0.5 inches (13 mm) in diameter, planes can be seriously damaged within seconds.^[38] The hailstones accumulating on the ground can also be hazardous to landing aircraft. Hail is also a common nuisance to drivers of automobiles, severely denting the vehicle and cracking or even shattering windshields and windows. Wheat, corn, soybeans, and tobacco are the most sensitive crops to hail damage.^[18] Hail is one of Canada's most expensive hazards.^[39] Rarely, massive hailstones have been known to cause concussions or fatal head trauma. Hailstorms have been the cause of costly and deadly events throughout history. One of the earliest recorded incidents occurred around the 9th century in Roopkund, Uttarakhand, India.^[40] The largest hailstone in terms of diameter and weight ever recorded in the United States fell on July 23, 2010 in Vivian, South Dakota; it measured 8 inches (20 cm) in diameter and 18.62 inches (47.3 cm) in circumference, weighing in at 1.93 pounds (0.88 kg).^[41] This broke the previous record for diameter set by a hailstone 7 inches diameter and 18.75 inches circumference (still the greatest circumference hailstone) which fell in Aurora, Nebraska in the United States on June 22, 2003, as well as the record for weight, set by a hailstone of 1.67 pounds (0.76 kg) that fell in Coffeyville, Kansas in 1970.^[41]

Accumulations[link]

Narrow zones where hail accumulates on the ground in association with thunderstorm activity are known as hail streaks or hail swaths,^[42] which can be detectable by satellite after the storms pass by.^[43] Hailstorms normally last from a few minutes up to 15 minutes in duration.^[22] Accumulating hail storms can blanket the ground with over 2 inches (5.1 cm) of hail, cause thousands to lose power, and bring down many trees. Flash flooding and mudslides within areas of steep terrain can be a concern with accumulating hail.^[44]

On somewhat rare occasions, a thunderstorm can become stationary or nearly so whilst prolifically producing hail and significant depths of accumulation do occur; this tends to happen in mountainous areas, such as the July 29, 2010 case of^[45] a foot of hail accumulation. Depths of up to a metre have been reported.

Suppression and prevention[link]

During the Middle Ages, people in Europe used to ring church bells and fire cannons to try to prevent hail, and the subsequent damage to crops. Updated versions of this approach are available as modern hail cannons. Cloud seeding after World War II was done to eliminate the hail threat,^[9] particularly across Russia - where it was claimed a 50 to 80 percent reduction in crop damage from hail storms was achieved by deploying silver iodide in clouds using rockets and artillery shells. Their results have not been able to be verified. Hail suppression programs have been undertaken by 15 countries between 1965 and 2005.^[18] To this day, no hail prevention method has been proven to work.^[9]

See also[link]

• Graupel
• Ice pellets
• Megacryometeor
• Snow grains

References[link]

Further reading[link]

• Rogers and Yau (1989). A Short Course in CLOUD PHYSICS. Massachusetts: Butterworth-Heinemann. ISBN 0-7506-3215-1. 
• Jim Mezzanotte (2007). Hailstorms. Gareth Stevens Publishing. ISBN 978-0-8368-7912-4. 
• Snowden Dwight Flora (2003). Hailstorms of the United States. Textbook Publishers. ISBN 978-0-7581-1698-7. 
• Narayan R. Gokhale (1974). Hailstorms and Hailstone Growth. State University of New York Press. ISBN 978-0-87395-313-9. 
• Duncan Scheff (2001). Ice and Hailstorms. Raintree Publishers. ISBN 978-0-7398-4703-9. 

External links[link]

Wikimedia Commons has media related to: Hail

Look up Hail or hail in Wiktionary, the free dictionary.

Wikisource has the text of the 1879 American Cyclopædia article Hail.

• Hail by income and population (Realtime)
• Hail Factsheet
• The Economic Costs of Hail Storm Damage NOAA Economics

Images

• Hail and hailstorms
• Major hail event in Brazil
• NOAA Hail Reports on Google map (non commercial)

Video

• Major Hail Storm in Calgary, Alberta, Canada, Aug.22,2010

Trey Songz
Background information
Birth name	Tremaine Aldon Neverson
Born	(1984-11-28) November 28, 1984 (age 27) Petersburg, Virginia, United States
Genres	R&B, hip hop
Occupations	Singer-songwriter, record producer, actor
Instruments	Vocals, keyboards, sampler
Years active	2004–present
Labels	Atlantic, Songbook
Associated acts	Drake, Troy Taylor, Twista, Juvenile, Bun B, Rick Ross, Plies
Website	www.treysongz.com

Tremaine "Trey" Aldon Neverson (born November 28, 1984), better known by his stage name Trey Songz, is an American singer-songwriter, rapper, record producer and actor. His debut album, I Gotta Make It, was released in 2005, while his second album, Trey Day, was released in 2007. His third album, Ready, was released in 2009 while his fourth studio album, Passion, Pain & Pleasure, was released on September 14, 2010.

Life and career[link]

1984–2004: Early life and career beginnings[link]

Songz was born Tremaine Aldon Neverson on November 28, 1984, in Petersburg, Virginia.^[1] Raised as a military brat, Songz did not have aspirations to have a musical career as a child due to his shyness, saying "Singing wasn't a reality for me, until other people started noticing I sounded good."^[2] He recognized his vocal abilities at the age of 14.^[2] Reluctant to sing, he began performing with encouragement by friends and family in high school. Record producer Troy Taylor discovered Songz during a talent show in 2000, which led him to signing a recording contract with Atlantic Records in 2002.^[2] After graduating from high school in 2002, Songz moved to New Jersey to begin recording his debut album, though recording didn't actually begin until 2003.^[1]

[edit] 2004–2008I Gotta Make It and Trey Day

While recording his debut album in 2004, Songz released multiple mixtapes under the alias Prince of Virginia.^[1] One of the mixtapes featured an "answer track" to R. Kelly's "Trapped in the Closet", entitled "Open the Closet". The song gave Trey some notoriety.^[3] His debut album, I Gotta Make It was released on July 26, 2005.^[4] It debuted at #20 on the Billboard 200, selling 40,000 copies in its first week of sales.^[5] It has sold 300,000 records in the US, but was never certified by the RIAA. Songz's debut single, Gotta Make It, featuring Twista, was released in March 2005 and reached #87 on the Billboard Hot 100 and #21 on the Hot R&B/Hip-Hop Songs. It garnered success in the R&B/urban community but failed to make a mark in mainstream music. The album's second and final single, Gotta Go, was released in July 2005 and reached #67 on the Hot 100 and #11 on the Hot R&B/Hip-Hop Songs chart, becoming even more successful than his debut single in the R&B/urban community and in the mainstream community. After promotion for his debut concluded, he was featured on the lead single from Twista's fifth album, The Day After. The single, "Girl Tonite", reached #14 on the Hot 100 and #3 on the Hot R&B/Hip-Hop Songs chart, becoming a huge hit.

Trey Songz performing in 2007.

In mid-2006, Songz began work on a follow-up album to his debut with longtime collaborator Troy Taylor and also employed hitmakers Bryan-Michael Cox, Danja, Stargate (production team) and R. Kelly to help create the album. Trey aimed for the album to be more mainstream-oriented than his debut album. His second studio album, Trey Day, was released on October 2, 2007. The album reached #11 on the Billboard 200,^[6] selling 73,000 copies in its first week. It has since sold 400,000 records in the US, becoming his second album not to be certified by the RIAA. The album was going to be released on May 8, 2007, but was continually delayed in order for a successful single to precede the album, as the lead single failed to impact charts.

His second album was preceded by the lead single, "Wonder Woman", which was released in February 2007. It reached #54 on the Hot R&B/Hip-Hop Songs chart, but failed to impact the Hot 100. Because of the single's failure, his second album was delayed from May 2007 to October 2007. The album's second single, "Can't Help but Wait", was released in August 2007 and was released to promote his second album and the film Step Up 2 the Streets soundtrack as a single for it. The single reached #14 on the Hot 100, and #2 on the Hot R&B/Hip-Hop Songs chart. It became Songz's first Top 20 hit on the Hot 100, and helped to boost his second album's sales. The single was also nominated for Best Male R&B Vocal Performance at the 2008 50th Grammy Awards. The third single from the album, "Last Time", was released in January 2008 and reached #69 on the Hot 100, and #9 on the Hot R&B/Hip-Hop Songs chart. The fourth and final single from the album, "Missin' You", was released in May 2008, but failed to chart completely. In mid-2008, Songz was nominated for a BET Award for Best Male R&B Artist but did not win the award.^[7]

[edit] 2009–2011: Ready and Passion, Pain & Pleasure

In late 2008, Trey began work on his third studio album with Bryan-Michael Cox, Sean Garrett, Stargate and Troy Taylor and aimed for the record to be more mature than his first two. Before releasing his third album, Songz released a mixtape titled Anticipation in June 2009 through his blog, which featured songs from his third album.^[8] Another mixtape from Trey was released in the summer of 2009, called Genesis. Genesis was a collection of Trey Songz's first recordings when he was fifteen years old and was released to show his fans the dedication that he had to making a record when he was young.^[9] Trey released his third studio album, Ready, on August 31, 2009. The album reached #3 on the Billboard 200, selling 131,000 copies in its first week.^[10] These are his best first week sales to date and the album was his first to reach the Top 10 on the Billboard 200. The album has since sold over 800,000 records in the US, earning a Gold certification from the RIAA in February 2010, becoming his first album to be certified by the RIAA.

Trey Songz performing at Summer Jam on June 5, 2010.

The lead single from the album, "I Need a Girl", was released in April 2009 and reached #5 on the Hot R&B/Hip-Hop songs chart and #59 on the Hot 100, becoming an R&B/urban hit but not a mainstream hit. A promotional single, "Successful", featuring rapper Drake, was released in June 2009 and reached #17 on the Hot 100, becoming Songz's third Top 20 hit. The single also served as the second and final single from Drake's EP, So Far Gone. The second official single from his third album, "LOL Smiley Face", featuring Soulja Boy Tell 'Em and Gucci Mane, was released in August 2009 and reached #51 on the Hot 100 and #12 on the Hot R&B/Hip-Hop Songs chart. The third single from the album, "I Invented Sex", featuring Drake, was released in October 2009 and reached #42 on the Hot 100 but #1 on the Hot R&B/Hip-Hop Songs chart, becoming his first single to top that chart. Like the first two singles from the album, it achieved success in the R&B/urban community but only some mainstream success. charted within the Billboard Hot 100, and topped the R&B chart. The fourth single from the album, "Say Aah", featuring rapper Fabolous, was released in January 2010 and reached #9 on the Hot 100 and #3 on the Hot R&B/Hip-Hop Songs chart. The single has become Trey's highest charting single on the Hot 100 and one of his most successful singles on the Hot R&B/Hip-Hop Songs chart.

The fifth and final single from the album, "Neighbors Know My Name", was released in February 2010 and reached #43 on the Hot 100 and #4 on the Hot R&B/Hip-Hop Songs chart. A sixth single, "Yo Side of the Bed", was going to be released in June 2010, but its release was canceled due to unknown reasons. A music video, featuring singer Keri Hilson, was filmed and released, however. Songz was also the opening act for Jay-Z on his Jay-Z Fall Tour in late 2009. The album was nominated for Best Contemporary R&B Album at the 52nd Grammy Awards in 2010, but lost to Beyoncé's I Am... Sasha Fierce. On April 1, 2010, he recorded an episode of MTV Unplugged, which aired on April 26, 2010.^[11] A documentary-series about Trey, Trey Songz: My Moment, began in June 2010 to positive reviews and high ratings. The 10-part series will end in August 2010 and follows Trey during his time as opening act on Jay-Z's Jay-Z Fall Tour in late 2009.

Songz's fourth studio album, Passion, Pain & Pleasure, was released on September 14, 2010.^[12] Trey began work on the album in early 2010 with Sean Garrett, Troy Taylor and Stargate and has stated that the album will be his most personal to date. The album was completed in July 2010. The album's lead single, "Bottoms Up", featuring female rapper Nicki Minaj, was released on July 27, 2010 and has reached number twenty-four on the Hot R&B/Hip-Hop Songs chart and was shared enough on Facebook to appear as a trending video on ItsTrending. Its video was filmed on July 31, 2010 and is pending release.^[13] Trey also filmed the video for the album's second single, "Can't Be Friends", on August 1, 2010.^[13] "Can't Be Friends" was released as the album's second single in August 2010.^[13] Songz embarked on the Passion, Pain & Pleasure Tour on August 6, 2010 with singer Monica. The tour is his first headlining tour to date and consists of shows in venues that seat 3,000 to 5,000 people. Songz also contributed the song "Already Taken" to the Step Up 3D soundtrack, which was released on July 27, 2010. He filmed a video for the song, which was released in July 2010. The leading lady in the video is former girlfriend and professional dancer Helen Gedlu. Songz appeared at the 2010 MTV Video Music Awards on September 12, 2010.^[14] Songz performed at BET Awards 2011 which broadcasted on June 26, 2011.^[15]

In July 2011, he was cast in The Texas Chainsaw Massacre 3D as Ryan, the male lead role.^[16]

[edit] 2011–present: Inevitable and Chapter 5

On August 18, 2011, it was announced Songz will be working on his fifth studio titled Chapter 5.^[17] In an interview Trey said the album, which will act as the follow-up to Passion, Pain & Pleasure, is said to be nearing completion. He also carried on to say "It’s my sixth year in the game so I’ve been here for a while now. You can expect the best me you’ve ever heard. I don’t have any release dates in mind right now but I’m just making music and enjoying myself in the studio and having fun. When I get to a place where I feel comfortable saying a date or all of that, people will definitely know. I have a few dream collaborations on that album that I want, but they say if you blow out your candle and make a wish you can’t tell people what you ask for or it won’t come true."^[18]

On November 28, 2011, on his birthday, Songz released his Inevitable EP to prepare for the release of his album. In February 2012, Songz will embark on his Anticipation 2our to promote his mixtape Anticipation 2 and to raise awareness of his new album.

Discography[link]

• I Gotta Make It (2005)
• Trey Day (2007)
• Ready (2009)
• Passion, Pain & Pleasure (2010)
• Chapter V (2012)

Tours[link]

• Passion, Pain & Pleasure Tour (headliner) (2010)
• OMG Tour (opening for Usher) (2010)
• Anticipation 2our (headliner) (2012)

Filmography[link]

Awards and nominations[link]

References[link]

External links[link]

Wikimedia Commons has media related to: Trey Songz

• Official website
• Trey Songz at the Internet Movie Database

Young Jeezy
Young Jeezy in 2006
Background information
Birth name	Jay Wayne Jenkins
Also known as	Lil J
Born	(1977-10-12) October 12, 1977 (age 34) Columbia, South Carolina[1]
Origin	Atlanta, Georgia, United States
Genres	Hip hop
Occupations	Rapper, songwriter
Years active	2001–present
Labels	CTE World/Def Jam, Def Jam South
Associated acts	USDA, Akon
Website	http://youngjeezy.defjam.com

Jay Wayne Jenkins (born October 12, 1977),^[1] better known by his stage name Young Jeezy, is an American rapper. He is a member of the hip hop group United Streets Dopeboyz of America (USDA) and a former member of BMF (Black Mafia Family). He began his career in 2001 under an independent label and joined Boyz 'N Da Hood in 2005, the same year his solo major label debut Let's Get It: Thug Motivation 101 was released. Its single "Soul Survivor", which featured Akon, became a top-ten hit in the US.

The Inspiration followed in 2006, and The Recession followed in 2008; both albums yielded chart-topping singles. Jeezy has also appeared on numerous other rap and R&B singles such as "Say I" by Christina Milian, "I'm So Paid" by Akon, "Hard" by Rihanna, and "Love in This Club" by Usher, the latter being a number one single on the US Billboard Hot 100 in 2008.

Early life[link]

Jay Wayne Jenkins was born in Columbia, South Carolina^[1] and relocated to Atlanta, Georgia when he was a toddler.^[2][3] Because his parents were separated, custody of him transferred between family members frequently. In an interview with XXL magazine, he described his childhood as "empty". In 1994, he spent nine months in YCA (Youth Challenge Academy), a boot camp in Fort Stewart, Georgia, for narcotics possession.^[4]

Music career[link]

Independent debut[link]

Jeezy released his first independent album, Thuggin' Under the Influence (T.U.I.), in 2001 under the name Lil J.^[5] It featured artists such as Freddy J.,Kinky B, Fidank, and Lil Jon, who also produced some of the tracks. In 2003, Jeezy released (also independently) Come Shop wit Me, a two CD set featuring completely new tracks with some songs from T.U.I. Jeezy signed with Bad Boy Records in 2004 and joined the group Boyz n da Hood, whose self-titled album was released in June 2005 and peaked at #5 on the Billboard 200 albums charts.

[edit] Let's Get It: Thug Motivation 101 (2005)

In May 2004, Jazze Pha's manager Henry 'Noonie' Lee showed Young Jeezy's demo to his friend Shakir Stewart, Vice President Artist and Repertoire (VP A&R) at Def Jam.^[6] Stewart "fell in love with it [the demo] the first time [he] heard it" and took it to L.A. Reid.^[6] Reid recognised the talent and gave Stewart the green light to sign him.^[6] As the "hottest thing on the street" at the time, various labels - including Warner and Interscope – were after his signature. However, Jeezy decided he wanted to be in business with Stewart and Reid. As a result, signed with Def Jam Records.^[6]

Jeezy's major label debut, Let's Get It: Thug Motivation 101, was released on July 26, 2005. He debuted at #2, selling 172,000 copies in its first week.^[7] It spawned several hit singles such as "Soul Survivor" featuring Akon. It reached #4 on the Billboard Hot 100 and #1 on the Hot Rap Tracks charts. "And Then What" featuring Mannie Fresh, which reached #67 on the Hot 100 and #13 on the Hot Rap Tracks. "My Hood", #19 on the Rap chart. In an interview with HitQuarters, A&R Shakir Stewart said that Jeezy had recorded over 60 songs for the album.^[6]

Jeezy partially wrote and performed on Gucci Mane's song, "Icy". Supposedly, Jeezy was never paid properly for his services. Those in Gucci Mane's camp have suggested that gang members from the Mechanicsville area attacked Gucci Mane to defend Jeezy's honor.^[8] Jeezy put out a track called "Stay Strapped" dissing Gucci Mane to the beat of "T.I.'s" song "A.S.A.P." Jeezy responded to Gucci Mane's, while rapping "even his own momma know, Radric Davis a bitch". In a recent Cutmaster C mixtape, The Hood News Page 3: Jay-Z Boycotts Cristal, Gucci disses Jeezy along with Jay Z in his track, "745". Jeezy addresses Gucci back on the same mixtape. While on the track "Break It Down", featuring Cmillz. On "Streets On Lock", from The Inspiration, Jeezy addressed Gucci Mane again, saying "What type of real nigga name himself after a bag?/Nigga you's a hoe, a Louis Vuitton fag". Towards the end of 2009, DJ Drama brought Young Jeezy to the radio station and called Gucci Mane to settle the beef once and for all. The two stopped feuding but throughout early 2010, the crews of Jeezy & Gucci (CTE & Brick Squad) have been in and out altercations with each other despite the fact Jeezy & Gucci have nothing to do with that. In 2011, Jeezy plans to release a new single featuring DJ Spluge and the rest of the Gangster Brigade.

In interviews and on several records, Jeezy has affirmed his resistance to commercialism in his music.^[9] Maintaining his street credibility, according to Jeezy, is of the utmost concern to him as an artist.^[4] In 2005, Jeezy was featured in several popular hip hop songs including Gucci Mane's "Icy"^[10] and Boyz n da Hood's "Dem Boyz". Due to having a successful solo career, he left the group. From time to time he still keeps in contact with a few of the members, but in early 2010 Jeezy & Jody Breeze (who is still a member of Boyz N Da Hood) began to diss each other which started a new beef between the two.

[edit] The Inspiration, U.S.D.A. (2006–2007)

In 2006, he was featured in Christina Milian's single "Say I". Jeezy's second major label album was The Inspiration, released in 2006. The album's first single "I Luv It" peaked at #14 on the Billboard Hot 100. "Bury Me A G" and "Go Getta" featuring R. Kelly, and "Dreamin’" featuring Keyshia Cole followed.

He also portrayed himself in the hip-hop fighting themed game Def Jam: Icon. In 2007, Jeezy released Cold Summer, an album by rap group USDA which consists of Jeezy, Blood Raw, Slick Pulla, 2Eleven and Boo Rossini.^{[citation needed]}

Jeezy presented a week-long toy drive and charity event series with his CTE family with the first annual Toyz n da Hood toy drive. The series presented 1,000 toys for 1,000 kids at various locations in Macon and Atlanta, which began on December 17, 2007, with the CTE Christmas Kickoff from 10 pm to 5 am at Club Miami. The toy giveaway took place in the Unionville neighborhood of Macon and at the Old Fourth Ward Community in Atlanta.^[11]

[edit] The Recession (2008)

His third album, The Recession, was released in 2008. "Put On" featuring Kanye West was the lead single, which also led to a Grammy Nomination for Best Rap performance by a duo, but it came short. Put On was followed by "Vacation", "Crazy World", "My President" with Nas, and "Who Dat" to complete the Recession's singles. Jeezy appeared on the R&B singles "Love in This Club" by Usher and "I'm So Paid" by Akon (also with Lil Wayne). "Love in This Club" peaked at #1 on the Billboard Hot 100. Later, he performed on Ciara's single "Never Ever", from her album Fantasy Ride.^[12]