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Elsevier

Advances in Geophysics

  • 1 Edición, Volumen 36 - 10 de noviembre de 1994
  • Última edición
  • Editores: Renata Dmowska, Barry Saltzman
  • Idioma: Inglés

From the Reviews of Previous Volumes"This series has provided workers in many fields with invaluable reference material and criticism."- SCIENCE PROGRESS"Should be on the bookshelf… Leer más

Descripción

From the Reviews of Previous Volumes"This series has provided workers in many fields with invaluable reference material and criticism."- SCIENCE PROGRESS"Should be on the bookshelf of every geophysicist."- PHYSICS TODAY"The entire series should be in the library of every group working in geophysics"- AMERICAN SCIENTIST

De interès para

Researchers in geoscience.

Índice

A.M. Forte and W.R. Peltier, The Kinematics and Dynamics of Poloidal(Toroidal Coupling in Mantle Flow: The Importance of Surface Plates and Lateral Viscosity Variations. A. Udias and E. Buforn, Seismotectonics of the Mediterranean Region. Subject Index.

Reseñas

Praise for the Series
"This series has provided workers in many fields with invaluable reference material and criticism."—SCIENCE PROGRESS

"Should be on the bookshelf of every geophysicist."—PHYSICS TODAY

"The entire series should be in the library of every group working in geophysics."—AMERICAN SCIENTIST

Detalles del producto

  • Edición: 1
  • Última edición
  • Volumen: 36
  • Publicado: 10 de noviembre de 1994
  • Idioma: Inglés

Sobre los editores

RD

Renata Dmowska

Renata Dmowska works in the School of Engineering and Applied Sciences at Harvard University in Cambridge, MA, USA.
Afiliaciones y experiencia
School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA

BS

Barry Saltzman

Barry Saltzman, 1932-2001, was professor of geology and geophysics at Yale University and a pioneer in the theory of weather and climate, in which he made several profound and lasting contributions to knowledge of the atmosphere and climate. Saltzman developed a series of models and theories of how ice sheets, atmospheric winds, ocean currents, carbon dioxide concentration, and other factors work together, causing the climate to oscillate in a 100,000-year cycle. For this and other scientific contributions, he received the 1998 Carl Gustaf Rossby Research Medal, the highest award from the American Meteorological Society. Saltzman was a fellow of the American Meteorological Society and the American Association for the Advancement of Science and an honorary member of the Academy of Science of Lisbon. His work in 1962 on thermal convection led to the discovery of chaos theory and the famous "Saltzman-Lorenz attractor."
Afiliaciones y experiencia
Yale University, New Haven, Connecticut, U.S.A.

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