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Titlebook: Advanced Ocean Modelling; Using Open-Source So Jochen K?mpf Book 2010 Springer-Verlag Berlin Heidelberg 2010 Climate Sciences.Computational

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期刊全稱Advanced Ocean Modelling
期刊簡(jiǎn)稱Using Open-Source So
影響因子2023Jochen K?mpf
視頻videohttp://file.papertrans.cn/147/146052/146052.mp4
發(fā)行地址Step-by-step introduction to more complex aspects of hydrodynamic modelling suitable for graduates and professional scientists.The books is also suitable for online teaching and external workshops.Inc
圖書(shū)封面Titlebook: Advanced Ocean Modelling; Using Open-Source So Jochen K?mpf Book 2010 Springer-Verlag Berlin Heidelberg 2010 Climate Sciences.Computational
影響因子This book focuses on motions of incompressible ?uids of a freely moving surface being in?uenced by both the Earth’s rotation and density strati?cation. In contrast to traditional textbooks in the ?eld of geophysical ?uid dynamics, such as those by by Cushman-Roisin (1994) and Gill (1982), this book uses the method of proce- oriented hydrodynamic modelling to illustrate a rich variety of ?uid phenomena. To this end, the reader can adopt the model codes, found on the Springer server accompanying this book, to reproduce most graphs of this book and, even better, to create animation movies. The reader can also employ the codes as templates for own independent studies. This can be done by a lay person as a hobby activity, undergraduate or postgraduate students as part of their education, or professional scientists as part of research. Exercises of this book are run with open-source software that can be freely downloaded from the Internet. This includes the FORTRAN 95 compiler “G95” used for execution of model simulations, the data visualisation program “SciLab”, and “ImageMagick” for the creation of graphs and GIF animations, which can be watched with most Internet browsers.
Pindex Book 2010
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書(shū)目名稱Advanced Ocean Modelling影響因子(影響力)




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Takuya Abe,Simon A. Levin,Masahiko Higashixercises address geostrophic adjustment of density fronts, coastal upwelling and Ekman pumping. The last exercise of this chapter explains the curiosity that winds can create flows in the ocean running opposite to the wind direction.
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https://doi.org/10.1007/978-1-4612-1906-4a strait, density-driven exchange flows through a strait, coastal upwelling in three dimensions, the thermohaline deep circulation in the ocean, and, as a highlight, equatorially trapped Kelvin waves accompanying El-Ni?o events.
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https://doi.org/10.1007/978-3-642-10610-1Climate Sciences; Computational Modelling; Geophysical Fluid Dynamics; Hydrodynamic Modelling; Marine En
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