Published 1967 | Version v1
Report

The variance of an increasingly smoothed random variable

Creators

  • 1. Pacific Northwest Lab., Atmospheric Sciences Section, Richland, Washington (United States)

Description

The rate of decrease of the variance of a stationary random function with increasing smoothing is examined from the viewpoint of the definition of variance. Assuming the smoothing interval, t, to be small with respect to the length of record, and the variance to be calculated from overlapping running means, it is shown that the variance, σ2s, is related to smoothing interval by dσ2s/σ22,o = 2 [P(t/2)/σ2s -1] dt/t where P(t/2) is the autocovariance at lag t/2. Semi-empirical forms for P(t/2) are shown to provide a good fit for results from time series of both Gaussian and non-Gaussian distributions, and to yield fair estimates of the autocovariance as a function of lag time. (author)

Part of:
Proceedings of the USAEC Meteorological Information Meeting

Additional details

Publishing Information

Imprint Title
Proceedings of the USAEC Meteorological Information Meeting
Imprint Pagination
630 p.
Journal Page Range
p. 426-436
Report number
AECL--2787

Conference

Title
USAEC Meteorological Information Meeting
Dates
11-14 Sep 1967
Place
Chalk River, Ontario (Canada)

INIS

Country of Publication
Canada
Country of Input or Organization
Canada
INIS RN
44096520
Subject category
S54: ENVIRONMENTAL SCIENCES;
Resource subtype / Literary indicator
Conference
Descriptors DEI
ATMOSPHERES; FLUCTUATIONS; MATHEMATICAL MODELS; POLLUTANTS; TURBULENCE
Descriptors DEC
VARIATIONS

Optional Information

Notes
10 refs., 4 figs.