Titlebook: Climate Dynamics of the Tropics; Stefan Hastenrath Book 1991 Kluwer Academic Publishers 1991 Atmospheric circulation.Climatology.Cloud.Inv

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https://doi.org/10.1007/3-540-29087-7descending portions of these cells and the associated anticyclonic axes in the lower troposhere provide a natural delineation of the poleward extremities of the tropical atmosphere. Accordingly, the discussion of regional circulation systems in this chapter will in Sections 6.3 to 6.6 proceed from t

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https://doi.org/10.1007/3-540-29087-7s to be concentrated. The purpose of the present chapter is to review the large-scale environmental setting, and the regional and seasonal characteristics of prominent synoptic weather systems. Atmospheric disturbances are individuals rather than identical replicas of each other. Synoptic models are

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Basic Physical and Mathematical Principles,ssed in Chapters 6 and 7, while Chapter 4 provides an orientation on the characteristic average mode of operation of the low-latitude oceans. This background is required for the understanding of year-to-year variations which are to be explored in the present chapter. The mechanisms of interannual va

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https://doi.org/10.1007/3-540-29087-7 directed at climatic and environmental change (UNESCO, 1970; World Meteorological Organization-ICSU, 1975, pp. 7, 11, 16; International Association of Hydrological Sciences -UNESCO, 1977; Temporary Technical Secretariat for World Glaciers Inventory, UNESCO-UNEP-IASH-ICSI, 1977; United Nations Envir

PANIC

Excursion in the World of Food Rheology,ime scale. This final chapter is a preliminary synopsis of climate and circulation conditions in the tropics in the geological past. The available field evidence limits this attempt mainly to the last 30 000 years. For the more distant past refer to the comprehensive review of Crowley (1983).

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Climate Dynamics of the Tropics978-94-011-3156-8Series ISSN 1383-8601 Series E-ISSN 2215-162X