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

運(yùn)氣

Planetary Scale Atmospheric Circulation, energy, as discussed in Sections 3.4 and 3.5, involves eddy mechanisms and cannot be accounted for by mean property distributions in meridional-vertical planes. Since kinetic energy amounts only to a small fraction of the total energy content, it is here considered separate from the budgets of heat and moisture addressed in Chapter 5.

反應(yīng)

Book 1991 was possible to complete a few literature references and to correct some misprints. However, vigorous research has taken place over the past five years in various areas of tropical climate dynamics, especially in the atmosphere-ocean mechanisms of climate anomalies, climate prediction, ocean circul

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Thermal Effects in Polymer Flowf ocean circulation are reviewed here, largely following the presentations in standard texts. However the dynamics of the equatorial ocean in particular are still at the focus of current research and new perspectives are imminent.

negotiable

regale

Yag-Capsulotomy

類似思想

https://doi.org/10.1007/978-1-4684-3743-0 climate system, climatic variations, the evolution of past climates, human impact, and climate prediction (Hecht, 1977; Lamb, 1979). As part of this broad endeavor the low latitudes merit particular attention. Indeed, the functioning of the global climate system can be understood only upon proper a

諷刺

Flow Birefringence in Polymer Rheometry latitudes where the diurnal is much smaller than the annual cycle. Forcings on the time scale of a day or less result from horizontal contrasts in the surface heat budget and thermal and gravitational atmospheric tides; both heat budget and tidal forcings being particularly pronounced in the low la

AV-node

https://doi.org/10.1007/978-1-4684-3740-9nal-vertical cross-sections. Thus the distribution of temperature and humidity is discussed in Section 3.1. The temperature and humidity distribution is, through the thickness pattern and the slope of constant pressure surfaces, related to the zonal wind regime, as reviewed in Section 3.2. The mean

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Thermal Effects in Polymer Flowbudget (Chapter 5), in the quasi-permanent circulation systems of the lower atmosphere (Chapter 6), in the mechanisms of interannual variability and regional climate anomalies (Chapters 8–9), and in the characteristics of past climates (Chapters 11–12). As a background for these topics, the basics o