Big From Wikipedia, the free encyclopedia Jump to: navigation, search For other uses, see Big (disambiguation). Big Promotional film poster for Big. Directed by Penny Marshall Produced by James L. Brooks Robert Greenhut Written by Gary Ross Anne Spielberg Starring Tom Hanks Elizabeth Perkins Robert Loggia John Heard Music by Howard Shore Cinematography Barry Sonnenfeld Distributed by 20th Century Fox Release date(s) June 3, 1988 (USA) Running time 104 min. Language English Budget $18,000,000 (est.) All Movie Guide profile IMDb profile Big is a 1988 comedy film about a teenage boy who is aged to adulthood by a magical fortune-telling machine. It stars Tom Hanks, Elizabeth Perkins, Robert Loggia, John Heard, Jared Rushton, David Moscow, Jon Lovitz and Mercedes Ruehl. The movie was written by Gary Ross, with Justin Schindler, and Anne Spielberg. Penny Marshall directed.
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Wind is the movement of Air (as opposed to an air current) caused by uneven heating of the Earth's surface. It occurs at all scales, from local breezes generated by heating of land surfaces and lasting tens of minutes to global winds resulting from solar heating of the Earth. The two major influences on the atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Given a difference in barometric pressure between two air masses, a wind will arise between the two which tends to flow from the area of high pressure to the area of low pressure until the two air masses are at the same pressure, although these flows will be modified by the Coriolis effect in the extratropics. Winds can be classified either by their scale, the kinds of forces which cause them (according to the atmospheric equations of motion), or the geographic regions in which they exist. There are global winds, such as the wind belts which exist between the atmospheric circulation cells. There are upper-level winds, such as the jet streams. There are synoptic-scale winds that result from pressure differences in surface air masses in the middle latitudes, and there are winds that come about as a consequence of geographic features such as the sea breeze. Mesoscale winds are those which act on a local scale, such as gust fronts. At the smallest scale are the microscale winds which blow on a scale of only tens to hundreds of meters and are essentially unpredictable, such as dust devils and microbursts. Winds can also shape landforms,
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