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Titlebook: Operational Oceanography in the 21st Century; Andreas Schiller,Gary B. Brassington Book 2011 Springer Science+Business Media B.V. 2011 atm

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41#
發(fā)表于 2025-3-28 16:57:10 | 只看該作者
Book 2011seen the development and implementation of operational ocean forecast systems?of the global ocean. At the conclusion of the Global Ocean Data Assimilation Experiment (GODAE) in 2008 ocean analysis and?forecasting services were being supported by 12 international centres..This book is about ocean for
42#
發(fā)表于 2025-3-28 21:10:12 | 只看該作者
43#
發(fā)表于 2025-3-29 01:36:53 | 只看該作者
In-Situ Ocean Observing Systemning to physical variables are described. A brief status on Indian Ocean Observing system (IndOOS) is also described. The strengths and weaknesses of each platform and the need for integrating different observational platforms/sensors are highlighted.
44#
發(fā)表于 2025-3-29 03:20:05 | 只看該作者
the last few years.Focuses on the Asian-Pacific region, with.Over the past decade the significant advances in real-time ocean observing systems, ocean modelling, ocean data assimilation and super-computing has seen the development and implementation of operational ocean forecast systems?of the globa
45#
發(fā)表于 2025-3-29 08:58:06 | 只看該作者
Ocean Data Quality Controltoring tool is emphasized, and some specific examples are given of new quality control techniques developed in numerical weather prediction that have direct applicability in ocean data assimilation and forecasting systems.
46#
發(fā)表于 2025-3-29 15:00:08 | 只看該作者
Observing System Design and Assessmentniques, including breeding, adjoint sensitivity, and singular vectors. In this chapter, the concepts for observing system design and assessment are introduced. A variety of different methods are then described, including examples of oceanographic applications of each method.
47#
發(fā)表于 2025-3-29 15:36:49 | 只看該作者
48#
發(fā)表于 2025-3-29 21:21:19 | 只看該作者
49#
發(fā)表于 2025-3-30 01:31:41 | 只看該作者
Tides and Internal Waves on the Continental Shelfography, and the intensity of the tidal forcing. The character of the near boundary flow in the region where waves are generated is very important in determining the internal wave response. When cyclones are present, the intense mixing over the water column can suppress the formation of tidally generated internal wave motions for many days.
50#
發(fā)表于 2025-3-30 07:49:57 | 只看該作者
978-94-017-7783-4Springer Science+Business Media B.V. 2011
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