Harmonic analysis: Difference between revisions
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|Meaning=#A [[statistical]] method for determining the [[amplitude]] and [[period]] of certain [[harmonic]] or [[wave]] components in a set of data with the aid of [[Fourier series]]. | |||
|Explanation=Harmonic analysis has been used in meteorology, for example, to determine periodicities in climatic data (Conrad 1950); to determine the wavelengths most strongly represented in [[general circulation|general circulation]] flow patterns; and to determine the [[spectrum]] of turbulent [[eddies]] (Sutton 1953).<br/> | |||
#The representation of tidal variations as the sum of several [[harmonics]], each of different [[period]], [[amplitude]], and [[phase]].<br/> The periods fall into three tidal species: long period, [[diurnal]], and semidiurnal. Each tidal species contains groups of harmonics that can be separated by analysis of a month of observations. In turn, each group contains constituents that can be separated by analysis of a year of observations. In shallow water, harmonics are also generated in the third-diurnal, fourth-diurnal, and higher species. These constituents can be used for [[harmonic prediction]] of tides.<br/> Conrad, V. 1950. Methods in Climatology. 119–154. <br/> Sutton, O. G. 1953. Micrometeorology. 96–103. | |||
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Latest revision as of 12:39, 30 March 2024
- A statistical method for determining the amplitude and period of certain harmonic or wave components in a set of data with the aid of Fourier series.
Harmonic analysis has been used in meteorology, for example, to determine periodicities in climatic data (Conrad 1950); to determine the wavelengths most strongly represented in general circulation flow patterns; and to determine the spectrum of turbulent eddies (Sutton 1953).
- The representation of tidal variations as the sum of several harmonics, each of different period, amplitude, and phase.
The periods fall into three tidal species: long period, diurnal, and semidiurnal. Each tidal species contains groups of harmonics that can be separated by analysis of a month of observations. In turn, each group contains constituents that can be separated by analysis of a year of observations. In shallow water, harmonics are also generated in the third-diurnal, fourth-diurnal, and higher species. These constituents can be used for harmonic prediction of tides.
Conrad, V. 1950. Methods in Climatology. 119–154.
Sutton, O. G. 1953. Micrometeorology. 96–103.