Nonlinear Sciences – Chaotic Dynamics
Scientist
Nonlinear Sciences
Chaotic Dynamics
Scientist
Department of Mathematics and Statistics, Queens University, Kingston, Ontario K7L 3N6, Canada
Center for Astrophysics, 60 Garden Street, Cambridge, Massachusetts 02138David J.ThomsonAT&T Bell Laboratories, 2C-360, Murray Hill, New Jersey 07974-2070 rschildatcfa.harvard.edu
AT & T Bell Laboratories, Murray Hill, New Jersey 07974, USA
AT&T Bell Labs., Murray Hill, NJ
Math and Statistics Department, Queen's University, Kingston, ON K7L3N6 Canada University, Kingston, Ontario, Canada
Mathematics and Statistics Department, Queens University, Kingston, ON, Canada
Dept. of Mathematics and Statistics, Queen's University, Kingston, ON, Canada;
Queen's University, Math and Statistics, Kingston, ON K7L 3N6 Canada
Queen's University, Department Math and Statistics Queen's University, Kingston, ON K7L 3N6 Canada
Department of Mathematics and Statistics, Queen's University, Jeffery Hall, University Avenue, Kingston, ON K7L 3N6 Canada
Queen's University, Mathematics and Statistics, Kingston, ON K7L 3N6 Canada
Queen's University, Department of Mathematics and Statistics 411 Jeffery Hall, KIngston, ON K7L 3N6, Canada
Queen's University, 411 Jeffery, Kingston, ON K7L 3N6 Canada
AT&T Bell Laboratories, Murray Hill, NJ
Department of Mathematics & Statistics, Queen's University, Kingston, ON, Canada
Bell Laboratories, Lucent Technologies, Room 1E439, 600 Mountain Avenue, Murray Hill, NJ 07974, USA Laboratories / Lucent Technologies, 600 Mountain Avenue, Murray Hill, NJ 07974, USA Laboratories, Lucent Technologies, 700 Mountain Avenue, Murray Hill, NJ 07974, USA N.J. USA
Meteorological Office, Bracknell, England
Bell Laboratories, Lucent Technologies, 600 Mountain Ave. Room 1E-439, Murray Hill, NJ 07974, USA
Queens University, 411 Jeffrey Hall Queen's University, Kingston, ON K7L 3N
40 Years of Solar Microwave Burst Flux Measurements
A Discussion of the Finite Difference Method in Computer Modelling of Electrical Conductivity Structures. A Reply to the Discussion by Williamson, Hewlett and Tammemagi
ACE to Ulysses Coherences
Bounded influence magnetotelluric response function estimation
Characteristics and Source of Unexpected Modes Observed in the Low Frequency Seismic Spectrum
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