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 interact
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 ...
The book will be of great use to scientists involved in the study of celestial bodies, such as astronomers and astrophysicists.
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 results of...
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” ...