Harmonic analysis: Difference between revisions

From Glossary of Meteorology
No edit summary
m (Rewrite with Template:Term and clean up)
 
Line 1: Line 1:
 
{{Term
 
|Display title=harmonic analysis
{{TermHeader}}
|Definitions={{Definition
{{TermSearch}}
|Num=1
 
|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]].
<div class="termentry">
|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/>  
  <div class="term">
#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&ndash;154. <br/> Sutton, O. G. 1953. Micrometeorology. 96&ndash;103.  
== harmonic analysis ==
}}
  </div>
}}
 
#<div class="definition"><div class="short_definition">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]].</div><br/> <div class="paragraph">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).</div><br/> </div>
#<div class="definition"><div class="short_definition">The representation of tidal variations as the sum of several [[harmonics]], each of different  [[period]], [[amplitude]], and [[phase]].</div><br/> <div class="paragraph">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.</div><br/> </div><div class="reference">Conrad, V. 1950. Methods in Climatology. 119&ndash;154. </div><br/> <div class="reference">Sutton, O. G. 1953. Micrometeorology. 96&ndash;103. </div><br/>
</div>
 
{{TermIndex}}
{{TermFooter}}
 
[[Category:Terms_H]]

Latest revision as of 12:39, 30 March 2024

  1. 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).

  1. 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.
Copyright 2025 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.