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By Adrian E. Gill

Applies successive bifurcations method of advanced time-dependent tactics in huge scale atmospheric dynamics, geomagnetism, and theoretical weather dynamics. Presentation of effects on planetary-scale phenomena within the earth's surroundings, ocean, cryosphere, mantle and center presents an built-in account of mathematical thought and strategies including actual phenomena and procedures. Brings jointly smooth instruments of nonlinear arithmetic and the issues of world swap within the atmosphere

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18. Salinity in summer (ppt). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). 19. Salinity in autumn (ppt). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). 40 The immediate past: A summary of the pre-desiccation state [Ch. 11. Long-term average monthly density t (kg/m 3 ) of Aral Sea water in Aralsk and Barsakelmes (1949±1960). Adapted from Bortnik and Chistyaeva (1990). 20. Surface density (t ) distribution in spring (kg/m 3 ).

Redrawn from Bortnik and Chistyaeva (1990). 12. Temperature in summer ( C). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). 13. Temperature in autumn ( C). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). Sec. 10. Basic statistics for surface salinity (ppt) in different months (1949±1960). The notation  is used for the root mean square deviation. The data were collected near Barsakelmes Island in the central part of the Sea.

Redrawn from Bortnik and Chistyaeva (1990). 24. Density t in summer (kg/m 3 ). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). 25. Density t in autumn (kg/m 3 ). Longitudinal vertical section through the western deep basin. Redrawn from Bortnik and Chistyaeva (1990). 44 The immediate past: A summary of the pre-desiccation state [Ch. 2 western basin and Chernyshev Bay. Minimum transparency (2±4 m on average) is observed in the southern part of the Sea adjacent to the Amu-Darya delta.

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