For advanced undergraduate and beginning graduate students in atmospheric, oceanic, and climate science, Atmosphere, Ocean and Climate Dynamics is an introductory textbook on the circulations of the atmosphere and ocean and their interaction, with an emphasis on global scales. It will give students a good grasp of what the atmosphere and oceans look like on the large-scale and why they look that way. The role of the oceans in climate and paleoclimate is also discussed. The combination of observations, theory and accompanying illustrative laboratory experiments sets this text apart by making it accessible to students with no prior training in meteorology or oceanography. * Written at a mathematical level that is appealing for undergraduates and beginning graduate students * Provides a useful educational tool through a combination of observations and laboratory demonstrations which can be viewed over the web * Contains instructions on how to reproduce the simple but informative laboratory experiments * Includes copious problems (with sample answers) to help students learn the material.
J. F., 109, l 10, 11, 112 Lyot, B., 160 M MacDonald, G. J. F., 292 McCartney, E. J., 159 McConnell, J. C., 115, 196, 207, 24! ... 43 Mintz, Y., 68,76 Mitra, S. K., 207 Mo, T., 295 Molina, M. J., 117 Moos, H. W., 240 Moshkin, B. E., 43, ...
Theory of Planetary Atmospheres: An Introduction to Their Physics and Chemistry
This book reviews the approach to the kinetic simulation of nonequilib rium processes in the planetary atmospheres which the authors developed and dealt with since the 1970s.
The other relations hold for homogeneous atmospheres. a: R* (su, pio, po – p) = R(p, plo, p – po) b: T'(u, u0, 20 - ?) = T(u, u0, 2 – 20) c: R(u0, u, p - 20) = AAR(u, u0, 2 - 20)A4 (I) d: T(u0, 11, p – po) = A3T(u, H0, p – po)A3 e: R(u ...
29(14), 1698 (2002). doi:10.1029/ 2002GL015044 R.G. Harrison, Long term measurements of the global atmospheric electric circuit at Eskdalemuir, Scotland, 1911–1981. Atmos. Res. 70(1), 1–19 (2004). doi:10.1016/ j.atmosres.2003.09.007 ...
The book will be of great use to scientists involved in the study of celestial bodies, such as astronomers and astrophysicists.
As mentioned earlier, the Proterozoic was warm during its middle part but extremely cold on both ends. Indeed, both the Paleoproterozoic and Neoproterozoic glaciations are thought by some geologists to have been “Snowball Earth” ...