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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
Providing an introduction to a branch of climate theory - the study of climate by means of the quality theory of partial differential equations, this text is oriented towards specialists and graduates in geophysical hydrodynamics and climate modelling. The first part of the book concentrates on current theory of infinite-dimensional and finite-dimensional nonlinear dissipative systems. Section two of the text contains the results of analysis of climate models of different complexity from barotropic models to models based on the full system of hydrothermodynamics equations.
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This title is printed to order. This book may have been self-published. If so, we cannot guarantee the quality of the content. In the main most books will have gone through the editing process however some may not. We therefore suggest that you be aware of this before ordering this book. If in doubt check either the author or publisher’s details as we are unable to accept any returns unless they are faulty. Please contact us if you have any questions.
Providing an introduction to a branch of climate theory - the study of climate by means of the quality theory of partial differential equations, this text is oriented towards specialists and graduates in geophysical hydrodynamics and climate modelling. The first part of the book concentrates on current theory of infinite-dimensional and finite-dimensional nonlinear dissipative systems. Section two of the text contains the results of analysis of climate models of different complexity from barotropic models to models based on the full system of hydrothermodynamics equations.