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Ocean Circulation, Second Edition

معرفی کتاب «Ocean Circulation, Second Edition» نوشتهٔ Open University; Angela Colling; Open University. Oceanography Course Team در سال 2001. این کتاب در فرمت pdf، زبان انگلیسی ارائه شده است. «Ocean Circulation, Second Edition» در دستهٔ بدون دسته‌بندی قرار دارد.

This second edition retains the general structure of the first edition, but has been updated in the light of recent oceanographic research, and improved as a teaching text on the basis of feedback from past students and other readers. Notable additions include new sections addressing the topic of numerical modelling, and more discussion of natural oscillations in the ocean-atmosphere system (previously confined to the El Nįo phenomenon). In particular, the Chapter on the North Atlantic now includes a discussion of the North Atlantic Oscillation, as well as of the Great Salinity Anomaly. In the final Chapter, treatment of water mass formation has been updated to reflect recent ideas about the processes involved and how they relate to climatic change over different time-scales, from decades to millennia. High quality full colour diagrams Substantial chapter summaries ideal for revision Answers, hints and notes for questions at back of the book. Read more... This second edition retains the general structure of the first edition, but
has been updated in the light of recent oceanographic research, and improved
as a teaching text on the basis of feedback from past students and other
readers.

Notable additions include new sections addressing the topic of
numerical modelling, and more discussion of natural oscillations in the
ocean-atmosphere system (previously confined to the El Niño phenomenon). In
particular, the Chapter on the North Atlantic now includes a discussion of
the North Atlantic Oscillation, as well as of the Great Salinity Anomaly. In
the final Chapter, treatment of water mass formation has been updated to
reflect recent ideas about the processes involved and how they relate to
climatic change over different time-scales, from decades to millennia.



High quality full colour diagrams
Substantial chapter summaries ideal for revision
Answers, hints and notes for questions at back of the book
« This second edition retains the general structure of the first edition, but has been updated in the light of recent oceanographic research, and improved as a teaching text on the basis of feedback from past students and other readers. Notable additions include new sections addressing the topic of numerical modelling, and more discussion of natural oscillations in the ocean-atmosphere system (previously confined to the El Niño phenomenon). In particular, the Chapter on the North Atlantic now includes a discussion of the North Atlantic Oscillation, as well as of the Great Salinity Anomaly. In the final Chapter, treatment of water mass formation has been updated to reflect recent ideas about the processes involved and how they relate to climatic change over different time-scales, from decades to millennia. High quality full colour diagrams Substantial chapter summaries ideal for revision Answers, hints and notes for questions at back of the book »-- Résumé de l'éditeur This second edition retains the general structure of the first edition, but has been updated in the light of recent oceanographic research, and improved as a teaching text on the basis of feedback from past students and other readers.Notable additions include new sections addressing the topic of numerical modeling, and more discussion of natural oscillations in the ocean-atmosphere system (previously confined to the El Nino phenomenon). In particular, the Chapter on the North Atlantic now includes a discussion of the North Atlantic Oscillation, as well as of the Great Salinity Anomaly. In the final Chapter, treatment of water mass formation has been updated to reflect recent ideas about the processes involved and how they relate to climatic change over different time-scales, from decades to millennia. The waters of the ocean are continually moving - in powerful currents like the Gulf Stream, in large gyres, in features visible from space (Figure 1.1), and in smaller swirls and eddies ranging in size down to a centimetre across or less.
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