chapter - Atmospheric and Oceanic Science
chapter - Atmospheric and Oceanic Science
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those of the future climate it is no longer valid.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