Titlebook: Climate Change in North America; George Ohring Book 2014 Springer International Publishing Switzerland 2014 Climate.Global Climate Change.

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Regional Climate Studieshttp://image.papertrans.cn/c/image/227538.jpg

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R. H. Adrian,E. Helmreich,A. Webern, North America has experienced a wide range of climates over time. The aim of this chapter is to review the history of those climate variations, focusing in particular on the continental-scale climatic variations between the Last Glacial Maximum (LGM, ca. 21,000?years ago or 21?ka) and the present

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https://doi.org/10.1007/BFb0031544e last 150 years or so, systematic, continuous instrumental measurements at weather stations have been the primary source of the climate record, as reviewed in Chap. 2. For the last fourdecades, observations of the Earth from space have provided a new source of information. This chapter focuses on t

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R. H. Adrian,E. Helmreich,A. Weberovide the data for geological time scales, weather station measurements cover the last 150?years or so, and satellite observations are available for the last four decades. This is the first of two chapters on the evaluation and use of computer models to simulate recent climate change in North Americ

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https://doi.org/10.1007/BFb0031544while adequate for resolving sub-continental North American climate features, is insufficient for simulating the more detailed properties of regional climate. To achieve higher resolution, a variety of so-called downscaling methods have been developed. This chapter reviews these methods and the resu

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https://doi.org/10.1007/BFb0034656American climate change (.) in response to human and natural influences. Taken together these simulations and observations provide evidence that North American climate has changed over recent decades, and that some of these changes are qualitatively consistent with those simulated in response to hum

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