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chapter - Atmospheric and Oceanic Science

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1.1. Dropping the hypothesis of stationary climate<br />

There is climate variability in almost all scales of time. In some of them, climatic<br />

variability come from processes of intrinsically r<strong>and</strong>om nature or are caused<br />

by multiple <strong>and</strong> complex processes that hamper its prediction. Hence, the use of the<br />

climate information is fundamentally based on the statistical analysis of its series.<br />

Up to not long ago, many of the uses of the climatic information, rested on the<br />

premise that the climate was stationary, at least at decadal scale, <strong>and</strong> so future climate<br />

would be similar to that of the immediate past. Therefore, the series of climatic<br />

elements <strong>and</strong> their hydrological derivates' were statistically treated as stationary.<br />

Nowadays, the hypothesis that climatic series or their derivates are stationary<br />

does not seem quite appropriate. Every time there are less doubts that the planet has<br />

entered in a rapid climatic change induced by human activities. In consequence the<br />

hypothesis almost always implicit that the statistics of the past climate can represent<br />

those of the future climate it is no longer valid. The whole methodological arsenal<br />

that was based on this simple presumption for the calculation of parameters of<br />

design of infrastructures, the planning of the use of the water resources, of the territory,<br />

of the forest activity or of the agriculture to medium term should be revised.<br />

In some regions <strong>and</strong> for certain parameters, the climatic series are already no<br />

longer stationary. For the cases that are still stationary, neither is a wise attitude to<br />

suppose, a priori <strong>and</strong> without further analysis, they will continue being so. In consequence,<br />

the estimate of some or several features of the future climate for some<br />

planning requirement can no longer relay in the comfortable hypothesis that the climate<br />

is stationary <strong>and</strong> therefore new methods are required. In spite of this necessity,<br />

there still is not a completely developed <strong>and</strong> sure methodology to estimate the<br />

future climate. Indeed, the great challenge for the world climatology during next<br />

years will be to develop the methods to predict the climate of next decades in view<br />

of the man induced climatic change.<br />

8<br />

CHAPTER<br />

INTRODUCTION<br />

Vicente Barros 1<br />

1 CIMA/CONICET. University of Buenos Aires.<br />

I

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