The Collected Papers of Lewis Fry Richardson: Volume 1Throughout his life Lewis Fry Richardson made many inspired contributions to various disciplines. Often his ideas were ahead of contemporary thinking, and preceded the technical means necessary for their practical implementation. He is best known for his wealth of important work on meteorology, and his groundbreaking application of mathematics to the causes of war, though his field of interest was in no way limited to these topics, and various aspects of psychology and mathematical approximation also benefited from his novel modes of thought. Collected in the first volume are all Richardson's important papers covering the mathematical and physical sciences. |
Contents
MEMOIRS OF THE ROYAL METEOROLOGICAL SOCIETY VOL I No | 2 |
The papers | 4 |
Introduction | 29 |
References | 47 |
The approximate arithmetical solution by finite differences of physical | 121 |
The approximate solution of various boundary problems by surface | 175 |
BY LEWIS F RICHARDSON | 201 |
CONTENTS | 233 |
km Mem R met Soc 1 116 | 553 |
THEOREM ON DRIFT OF HOT AND COLD | 578 |
GEOGRAPHICAL DISTRIBUTION OF THE HEIGHTINTEGRAL OF PRESSURE | 589 |
An absolute currentbalance having a simple approximate theory Proc | 723 |
Contents of Volume 1 | 757 |
Quanta and diffusion Unpublished MS | 811 |
mosses only as far as the saturated substance is concerned that | 864 |
THE SINGLELAYER PROBLEM | 897 |
PAGE | 247 |
irregularly Proc Lond math Soc 2 20 21112 | 311 |
Distribution of wars in time Nature Lond 155 610 | 375 |
Academy Nature Lond 159 269 | 413 |
Note on the patents | 995 |
1011 | |
Checklist of publications not reproduced in either volume 761 | 1015 |
Common terms and phrases
angle approximation arithmetic atmosphere axis balloon boundary centimetre centre chequer cloud co-ordinate coefficients coil constant correct corresponding curve denote density diagram diameter differential equations diffusion distance eddies eddy-diffusion elementary divisors equal error finite differences formula frequency function G. I. Taylor GEOSTROPHIC APPROXIMATION given graph height horizontal increase integral kilom L. F. Richardson latent column latent roots LEWIS F linear mass mathematical matrix mean measured Meteorological method metres metres per second molecules motion observations obtained oscillations oscillograph Osglim Lamp P₁ pair paper particles Phil physics plane position pressure problem Proc range ratio Royal Meteorological Society shown shows solution speed square standard deviation stress surface temperature theory thermometer tilt time-marks turbulence values vanish velocity vertical voltage wind zero