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Modal View of Atmospheric Variability - Applications of Normal-Mode Function Decomposition in Weather and Climate Research... Modal View of Atmospheric Variability - Applications of Normal-Mode Function Decomposition in Weather and Climate Research (Hardcover, 1st ed. 2020)
Nedjeljka Zagar, Joseph Tribbia
R2,738 Discovery Miles 27 380 Ships in 12 - 17 working days

This book reviews the theory and applications of the normal-mode functions in numerical weather prediction and weather and climate dynamics. The normal-mode functions, the eigensolutions of the linearized primitive equations describing the evolution of atmospheric winds and mass variables, have been used for a long time. They have played an important role in the development of data assimilation schemes and the initialization of numerical weather prediction models. Chapters also present how the normal modes can be applied to many theoretical and numerical problems in the atmospheric sciences, such as equatorial wave dynamics, baroclinic instability, energy transfers, and predictability across scales.

Modal View of Atmospheric Variability - Applications of Normal-Mode Function Decomposition in Weather and Climate Research... Modal View of Atmospheric Variability - Applications of Normal-Mode Function Decomposition in Weather and Climate Research (Paperback, 1st ed. 2020)
Nedjeljka Zagar, Joseph Tribbia
R2,800 Discovery Miles 28 000 Ships in 10 - 15 working days

This book reviews the theory and applications of the normal-mode functions in numerical weather prediction and weather and climate dynamics. The normal-mode functions, the eigensolutions of the linearized primitive equations describing the evolution of atmospheric winds and mass variables, have been used for a long time. They have played an important role in the development of data assimilation schemes and the initialization of numerical weather prediction models. Chapters also present how the normal modes can be applied to many theoretical and numerical problems in the atmospheric sciences, such as equatorial wave dynamics, baroclinic instability, energy transfers, and predictability across scales.

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