The high predictability of the atmosphere and ocean depends on the
existence of a 'slow manifold', which contains the solutions of
equations describing only large-scale motions. This unique
compendium succinctly describes major recent advances in showing
that these equations can be solved independently.The book is a new
edition of a similar book published 15 years ago. The explanation
of the mathematical techniques has been expanded. Many new
theoretical results are included. Illustrations derived from
production atmosphere and ocean models are also incorporated to
cover the full range between rigorous mathematics and
state-of-the-art numerical modelling.The author is a dynamical
meteorologist with long experience and international standing. The
mathematical results in the book were proved by many of the world's
leading analysts. The results come from the Met Office Unified
Model, which is one of the world's leading weather and climate
models.Related Link(s)
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