All About the Weather (Dover Pictorial Archives) by By (author) Bruce LaFontaine

By By (author) Bruce LaFontaine

Fun-to-color photos and targeted captions introduce school-age childrens to tornadoes, hurricanes, blizzards, and different atmospheric stipulations. rigorously researched illustrations and accompanying textual content depict and clarify cloud varieties, thunderstorm formation, worldwide wind styles and ocean currents, radar climate tools, and different phenomena. forty four black-and-white illustrations.

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4 Historical Development Climate models emerged from models that were developed for weather prediction since around 1940. Modelling atmospheric processes and circulation is the cradle of climate model development. Vilhelm Bjerknes (1862–1951, Fig. 6) was the first Fig. 6 Vilhelm Bjerknes (1862–1951), founder of dynamical meteorology. 4 Historical Development 11 Fig. 7 Lewis Fry Richardson (1881–1953) computed the first weather forecast. to realize that weather prediction was a problem of mathematics and physics.

The computations show that after a permitted maximum in 2030, the emissions need to decrease drastically (globally around 1% per year). Such model simulations are of crucial significance to global political decisions related to international treaties such as the Kyoto-Protocol and its successors. 5 Prediction of the Weak El Niño of 2002/2003 The irregular warming of waters in the tropical Eastern Pacific, known as the El Niño-Southern Oscillation (ENSO) phenomenon, strongly affects the tropical climate and in particular the water cycle.

1. 1 Hierarchy of Physical Climate Models 29 Fig. 2 Schematic illustration of model grids in three-dimensional AGCMs and OGCMs. The resolution of a coupled climate model is typically set at 4ı 4ı to 2ı 2ı and 20–40 vertical layers. 1ı are applied. In this case, the calculation is restricted to either limited regions or an extremely short time of integration, hence not yet applicable for global climate studies. Figures from Ruddiman (2007). results. Although such models are already run on personal computers or clusters, for their integration period quite strong limitations exist.

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