Revisiting Klima
Revisiting Klima
复制标题
重温克利马
作者:
James Rodger Fleming;V. Jankovic
We have named this volume Klima. (“κλίμα period”). This terse but dynamic moniker fi ts the tone of the contributions, which revive a multivocal and inclusive understanding of a venerable but elusive term. We seek to decouple Klima from its current exclusive association with atmospheric sciences and revisit the implications of an ancient vocabulary for medical, geographical, agricultural, economic, racial, and other “endemic” concerns. If climate is not just about the weather, what is it? What does it seek to explain? When is climate invoked? By whom? For what purposes? How are other “key words” linked with it, such as culture, society, civilization, time, and change? In what ways is climate a proxy for other concerns such as regulation, industry, and identity? When is it not an explanation at all? Where is climate incarnated? And how does it matter? Modern scientifi c climatology cannot answer these questions. Yet it is burdened with the enormous challenge of delineating how climate relates to social and economic life. This is perhaps inevitable, given that the defi nition of climate abstracts it from the “lived” experience and constructs it as a derived entity, a statistical index of averaged parameters across space and time. In 1897, the preeminent Austrian meteorologist Julius Hann wrote that “by climate we mean the sum total of the meteorological phenomena that characterize the average condition of the atmosphere at any one place on the earth’s surface.”1 According to Karl SchneiderCarius, the pioneering weather pilot and meteorologist, “Climatology is concerned with the average states of weather, and the frequency of the different individual types of weather in their geographical distribution.”2 More recently, the World Meteorological Organization defi ned climate “as the ‘average weather,’ or more rigorously, as the statistical description in terms of the mean and variability of relevant quantities over a period of time ranging from months to thousands or millions of years.”3 In a broader, scientifi c