The application of the scale autocorrelation coefficient to the determination of the harmonic content of periodic phenomena - a meteorological and a geophysical example

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050 4 ‡aQC807 .5 ‡b.U55 no. 408
086 0 ‡aD 301.45/39:408
088 ‡aAD 0750476
088 ‡aAFCRL 72-476
100 1 ‡aCorbin, Victor L.
245 1 4 ‡aThe application of the scale autocorrelation coefficient to the determination of the harmonic content of periodic phenomena - a meteorological and a geophysical example / ‡cV.L. Corbin, H.E. Moses, A.F. Quesada.
264 1 ‡aL.G. Hanscom Field, Bedford, Massachusetts : ‡bAir Force Cambridge Research Laboratories, Office of Aerospace Research, United States Air Force, ‡c1972.
300 ‡avi, 19 pages : ‡billustrations ; ‡c28 cm.
336 ‡atext ‡btxt ‡2rdacontent
337 ‡aunmediated ‡bn ‡2rdamedia
338 ‡avolume ‡bnc ‡2rdacarrier
490 0 ‡aAFCRL ; ‡v72-476
490 0 ‡aEnvironmental research papers ; ‡vNo. 408
500 ‡aResearch supported by the Air Force Cambridge Research Laboratories, Air Force Systems Command, United States Air Force, L.G. Hanscom Field, Bedford, Massachusetts.
500 ‡aAeronomy Laboratory, Project 7635.
500 ‡aAD0750476 (from http://www.dtic.mil).
500 ‡a"10 August 1972."
504 ‡aIncludes bibliographical references (page 19).
520 ‡aIn a previous work a scale autocorrelation coefficient was introduced that compares a function of time with itself when the scale of time is 'stretched. It was shown that the scale autocorrelation could be used to determine ratios of frequencies which occur in phenomena with periodicities. In the present paper the authors review the properties of the scale autocorrelation coefficient and apply it to the finding of some of the ratios of the frequencies in atmospheric pressures measured daily for 8766 days. The authors also apply it to the measurements of the International Magnetic Character Figure, C(i), which was measured daily for 27,258 days. The authors regard these applications as the first test of the utility of the scale autocorrelation coefficient. The results indicate that the scale autocorrelation coefficient may indeed prove to be a valuable supplement to the use of the usual autocorrelation coefficient and the Fourier transformation of time-dependent functions. (Author).
538 ‡aMode of access: Internet.
650 0 ‡aGeophysics ‡xMeteorology.
650 0 ‡aFourier analysis. ‡0http://id.loc.gov/authorities/subjects/sh85051088
650 0 ‡aHarmonic analysis. ‡0http://id.loc.gov/authorities/subjects/sh85058939
650 0 ‡aAutocorrelation (Statistics) ‡0http://id.loc.gov/authorities/subjects/sh85010059
700 1 ‡aQuesada, Antonio F.
700 1 ‡aMoses, H. E.
710 2 ‡aAir Force Cambridge Research Laboratories (U.S.) ‡0http://id.loc.gov/authorities/names/n81133515 ‡1http://id.loc.gov/rwo/agents/n81133515
730 0 ‡aTechnical Report Archive & Image Library (TRAIL)
899 ‡a39015095142561
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