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The turbines were replaced by four geared Kampon turbines with a designed output of 80,000 shp (60,000 kW) intended to increase their speed to 24.5 knots (45.4 km/h; 28.2 mph). [1] The fuel storage of the ships was increased which gave them a range of 7,870 nautical miles (14,580 km; 9,060 mi) at 16 knots (30 km/h; 18 mph), despite the ...
Full Speed may refer to: Full Speed, silent film western; Full Speed, Italian comedy film; Full Speed, French film; Full Speed, the album by Kid Ink; Full speed or flank speed, a nautical term referring to a ship's true maximum speed
Long Island was laid down on 7 July 1939, as the C-3 cargo liner Mormacmail, under Maritime Commission contract, by the Sun Shipbuilding and Drydock Company, Chester, Pennsylvania as Yard No 185, launched on 11 January 1940, sponsored by Ms. Dian B. Holt, acquired by the Navy on 6 March 1941, and commissioned on 2 June 1941 as Long Island (AVG-1), Commander Donald B. Duncan in command.
USS John Paul Jones (DDG-53) is the third Arleigh Burke-class guided missile destroyer in the United States Navy and the first ship of the class homeported on the west coast. . She is the fifth ship named after American Revolutionary War naval captain John Paul Jones and the second to carry his first na
Battle off Samar; Part of the Battle of Leyte Gulf, Philippines Campaign (1944–45), Pacific War (World War II): The escort carrier Gambier Bay, burning from earlier gunfire damage, is bracketed by a salvo from a Japanese cruiser (faintly visible in the background, center-right) shortly before sinking during the Battle off Samar.
USS Miguel Keith (ESB-5) (formerly USNS Miguel Keith (T-ESB-5)) is a Lewis B. Puller-class expeditionary mobile base, one of three such ships in service with the United States Navy (USN) as of late 2021.
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The rear flank downdraft can arise owing to negative buoyancy, which can be generated by cold anomalies produced at the rear of the supercell thunderstorm by evaporative cooling of precipitation or hail melting, or injection of dry and cooler air in the cloud, and by vertical perturbation pressure gradients that can arise from vertical gradients of vertical vorticity, stagnation of ...