GLOBAL WARMING AND THE PROBLEM OF TESTING FOR TREND IN TIME-SERIES DATA

Citation
Wa. Woodward et Hl. Gray, GLOBAL WARMING AND THE PROBLEM OF TESTING FOR TREND IN TIME-SERIES DATA, Journal of climate, 6(5), 1993, pp. 953-962
Citations number
23
Categorie Soggetti
Metereology & Atmospheric Sciences
Journal title
ISSN journal
08948755
Volume
6
Issue
5
Year of publication
1993
Pages
953 - 962
Database
ISI
SICI code
0894-8755(1993)6:5<953:GWATPO>2.0.ZU;2-0
Abstract
In recent years a number of statistical tests have been proposed for t esting the hypothesis that global warming is occurring. The standard a pproach is to examine one or two of the more prominent global temperat ure datasets by letting Y(t) = a + bt + E(t) where Y(t) represents the temperature at time t, and E(t) represents error from the trend line, and to test the hypothesis that b = 0. Several authors have applied t hese tests for trend to determine whether or not a significant long-te rm or deterministic trend exists, and have generally concluded that th ere is a significant deterministic trend in the data. However, we show that certain autoregressive-moving average (ARMA) models may also be very reasonable models for these data due to the random trends present in their realizations. In this paper, we provide simulation evidence to show that the tests for trend detect a deterministic trend in a rel atively high percentage of realizations from a wide range of ARMA mode ls, including those obtained for the temperature series, for which it is improper to forecast a trend to continue over more than a very shor t time period. Thus, we demonstrate that trend tests based on models s uch as Y(t) = a + bt + E(t) for the purpose of prediction or inference concerning future behavior should be used with caution. Of course, th e projections that the warming trend will extend into the future are l argely based on such factors as the buildup of atmospheric greenhouse gases. We have shown here, however, that based solely on the available temperature anomaly series, it is difficult to conclude that the tren d will continue over any extended length of time.