On the algebraic expression of the diurnal variation of temperature

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Abstract
Chapter vi, of tile" Anales de la Oficina hleteorologica Argentina," by the author.* The curiolls numerical vailles upou p. GO of Dr. Wild's "Temperatur-Y.erhiiltnissedes Russischen Reiches " from which it is inferred that the leg-itimate results from twenty.foll!' equidistant observatious callnot be fully represented by a formula containing twellty-four constants, are vitiated by the joint effect of an erl'01' of computation and the employment of an insutlicient number of decimals.The effect of these errors is quite insignificIUlt, it is true, and amounts to only a very few hundl'cdths of a degree j but it is precisely upon these small quantities, much inferior ill magnitude to the unavoidable errol'S of ollservation, that the whole argument of the author depends.* These, although iusignificant in themselves.are in fact sufficient to change the corresponding epoch of maximum by thirteen minlltes, or from 14h 15m to 14b 28m
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Authors B. A. Gould
Journal american journal of science
Year 1882
DOI
10.2475/ajs.s3-23.134.99
URL
https://doi.org/10.2475/ajs.s3-23.134.99
Keywords Keywords not found

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