The Jule G. Charney Award
The procedure for Awards nominations is restricted to electronic submissions, unless stated otherwise. The nominator is responsible for uploading the entire nomination package. Most awards require the following: nomination letter, nominee Curriculum Vitae, bibliography, and three (3) letters of support. Please allow sufficient time prior to the deadline to gather all required files.
The Atmospheric Research Awards Committee has the responsibility to select and submit to the Council the names of individuals nominated for this award. All nominations should be submitted by 1 May 2015. The nominees for most awards remain on the committee's active list for three years. Read More
The Jule G. Charney Award is granted to individuals in recognition of highly significant research or development achievement in the atmospheric or hydrologic sciences. The award is in the form of a medallion. Nominations are considered by the Atmospheric Research Awards Committee, which makes recommendations for final approval by AMS Council.
Jule Gregory Charney (1917–1981)
Jule Gregory Charney played a pivotal role in the development of modern meteorology.
Born in San Francisco in 1917, he studied physics at UCLA, where he earned a PhD in 1946. In the early 1950’s, he worked with John von Neumann at the Institute for Advanced Study at Princeton University, where they conducted pioneering research in numerical weather prediction using early computers.
Charney also formulated a set of equations (the quasigeostrophic set) for calculating the large-scale motions of planetary-scale waves. He gave the first convincing physical explanation for the development of mid-latitude cyclones known as the Baroclinic Instability theory.
From 1956 until his death in 1981, Jule Charney was a faculty member at the Massachusetts Institute of Technology.
In 1979 Charney chaired an "ad hoc study group on carbon dioxide and climate" for the National Research Council. The resulting report, "Carbon dioxide and climate: A scientific assessment", is one of the earliest modern scientific assessments of global warming.