back to earth is known as the critical frequency, and has a definite diurnal variation. The graphs of the E and F1 critical frequencies are symmetrical about the noon axis. This is not true of the F2 critical frequency, which, moreover, is much more variable. Comparison of the seasonal variations
Measurement of Lenard Rays
- Publisher
- Elsevier Science
- Year
- 1931
- Tongue
- English
- Weight
- 102 KB
- Volume
- 212
- Category
- Article
- ISSN
- 0016-0032
No coin nor oath required. For personal study only.
β¦ Synopsis
In order to compute the dominant wave-length and purity of a color stimulus by means of the "excitation" data of the Optical Society of America, two values must be obtained by interpolation. The adoption of the osculatory formula for this interpolation permits the computations to be made with perfect reproducibility. Each of the O. S. A. curves by this method is represented as a series of parabolas of the fifth degree which join at the values specified at every IO millimicrons so as to have a common slope and curvature at the junction point. Interpolated values have been computed according to this formula for every millimicron. Tables giving these data will be published in the July number of the Bureau of Standards Journal of Research.
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