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In 1956, Norman Phillips developed a mathematical model which could realistically depict monthly and seasonal patterns in the troposphere, which became the first successful [[General circulation model]] of climate.<ref name="Harper 2009 p. 113">{{cite book | last=Harper | first=K. | title=Weather and Climate: Decade by Decade | publisher=Facts On File, Incorporated | series=Facts on File science library | year=2009 | isbn=978-1-4381-0982-4 | url=http://books.google.com/books?id=zCmB1QLcO5IC&pg=PA113 | accessdate=March 15, 2015 | page=113}}</ref> He was awarded a [[Benjamin Franklin Medal (Franklin Institute)]] in 2003.
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In 1956, Norman Phillips developed a mathematical model which could realistically depict monthly and seasonal patterns in the troposphere, which became the first successful [[General circulation model]] of climate. He was awarded a [[Benjamin Franklin Medal (Franklin Institute)]] in 2003.


==Reference==
==Reference==

Revision as of 01:46, 15 March 2015

In 1956, Norman Phillips developed a mathematical model which could realistically depict monthly and seasonal patterns in the troposphere, which became the first successful General circulation model of climate.[1] He was awarded a Benjamin Franklin Medal (Franklin Institute) in 2003.

Reference

1. Phillips, Norman A. (April 1956). "The general circulation of the atmosphere: a numerical experiment". Quarterly Journal of the Royal Meteorological Society 82 (352): 123–154. Bibcode:1956QJRMS..82..123P. doi:10.1002/qj.49708235202. 2. Cox, John D. (2002). Storm Watchers. John Wiley & Sons, Inc. p. 210. ISBN 0-471-38108-X.

  1. ^ Harper, K. (2009). Weather and Climate: Decade by Decade. Facts on File science library. Facts On File, Incorporated. p. 113. ISBN 978-1-4381-0982-4. Retrieved March 15, 2015.