Book contents
- Frontmatter
- PREFACE
- Contents
- Chronological List of Papers with References to the Volumes in which they are contained
- Errata
- PART I PERIODIC ORBITS
- PART II THE TIDES
- PART III MISCELLANEOUS PAPERS IN CHRONOLOGICAL ORDER
- 5 On some Proposed Forms of Slide-rule
- 6 An Application of Peaucellier's Cell
- 7 The Mechanical Description of Equipotential Lines
- 8 On a Mechanical Representation of the Second Elliptic Integral
- 9 On Maps of the World
- 10 A Geometrical Puzzle
- 11 A Geometrical Illustration of the Potential of a Distant Centre of Force
- 12 On Graphical Interpolation and Integration
- 13 On a Theorem in Spherical Harmonic Analysis
- 14 On Fallible Measures of Variable Quantities, and on the Treatment of Meteorological Observations
- 15 On the Horizontal Thrust of a Mass of Sand
- 16 On the Formation of Ripple-mark in Sand
- 17 Note on Mr Davison's Paper on the Straining of the Earth's Crust in Cooling
- 18 On the Mechanical Conditions of a Swarm of Meteorites, and on Theories of Cosmogony
- 19 On the Perturbation of a Comet in the Neighbourhood of a Planet
- 20 The Eulerian Nutation of the Earth's Axis
- 21 The Analogy between Lesage's Theory of Gravitation and the Repulsion of Light
- PART IV PAPERS ON TIDES (Supplementary to Volume I)
- PART V ADDRESSES TO SOCIETIES
- APPENDIX
- INDEX
- Plate section
14 - On Fallible Measures of Variable Quantities, and on the Treatment of Meteorological Observations
Published online by Cambridge University Press: 07 September 2010
- Frontmatter
- PREFACE
- Contents
- Chronological List of Papers with References to the Volumes in which they are contained
- Errata
- PART I PERIODIC ORBITS
- PART II THE TIDES
- PART III MISCELLANEOUS PAPERS IN CHRONOLOGICAL ORDER
- 5 On some Proposed Forms of Slide-rule
- 6 An Application of Peaucellier's Cell
- 7 The Mechanical Description of Equipotential Lines
- 8 On a Mechanical Representation of the Second Elliptic Integral
- 9 On Maps of the World
- 10 A Geometrical Puzzle
- 11 A Geometrical Illustration of the Potential of a Distant Centre of Force
- 12 On Graphical Interpolation and Integration
- 13 On a Theorem in Spherical Harmonic Analysis
- 14 On Fallible Measures of Variable Quantities, and on the Treatment of Meteorological Observations
- 15 On the Horizontal Thrust of a Mass of Sand
- 16 On the Formation of Ripple-mark in Sand
- 17 Note on Mr Davison's Paper on the Straining of the Earth's Crust in Cooling
- 18 On the Mechanical Conditions of a Swarm of Meteorites, and on Theories of Cosmogony
- 19 On the Perturbation of a Comet in the Neighbourhood of a Planet
- 20 The Eulerian Nutation of the Earth's Axis
- 21 The Analogy between Lesage's Theory of Gravitation and the Repulsion of Light
- PART IV PAPERS ON TIDES (Supplementary to Volume I)
- PART V ADDRESSES TO SOCIETIES
- APPENDIX
- INDEX
- Plate section
Summary
If we make any observation, for example the transit of a star, a definite numerical result is obtained. To say that that result is liable to errors of observation, is only correct from one point of view. It is true that the result does not really correspond with the time at which the star crossed the meridian, yet it is an accurate representation of a certain very complex event. Undoubtedly, the principal feature in that event is the time of crossing the meridian; but there is also involved in it various properties of the instruments, the atmosphere, and the observer himself, &c. The object of the observation is, of course, to get a result which shall represent that principal feature, after the elimination of the minor features. The comparative simplicity of this, and of many other observations, permits us to unravel the complex event into its constituent parts, and to estimate each numerically. One part consists of corrections of all sorts. But when all these have been made, there still remains a result representing a complex event, viz. the transit of the star, together with unknown properties of the circumstances of the observation. These unknown properties form the subject-matter of the theory of errors of observation; but it is only because there is a consistent theory of the principal phenomenon, that the most probable line of demarcation can be drawn between the two parts of the complex event.
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- The Scientific Papers of Sir George DarwinPeriodic Orbits and Miscellaneous Papers, pp. 292 - 304Publisher: Cambridge University PressPrint publication year: 2009First published in: 1911