Abstract
Abstract Eigenvectors may be used in the same way as orthogonal polynomials. They have an advantage over those orthogonal functions expressible by simple formulas, however, in that they are derived from the data being studied and strongly resemble the important features of the data, so that the first several eigenvectors contain a much higher percentage of “variance” than would be contained in an equal number of ordinary orthogonal polynomials. This paper describes the process by which a matrix of eigenvectors was derived from the sets of 12 mean-monthly precipitation values for 60 stations in Nevada. The first three eigenvectors (in order of importance) were found to account for 93% of the “variance” in the original 12 × 60 matrix of raw data and they are also found to have features in common with three natural cycles of annual precipitation in Nevada. The effect of station elevation on each eigenvector is determined by linear correlation. The station multipliers, corrected to a mean elevation, are plott...
Cite
CITATION STYLE
Stidd, C. K. (1967). The Use of Eigenvectors for Climatic Estimates. Journal of Applied Meteorology, 6(2), 255–264. https://doi.org/10.1175/1520-0450(1967)006<0255:tuoefc>2.0.co;2
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