Changeset 14789 for NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/doc/latex/NEMO/subfiles/chap_model_basics.tex
- Timestamp:
- 2021-05-05T13:18:04+02:00 (3 years ago)
- Location:
- NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU
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- 3 edited
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NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU
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NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/doc/latex/NEMO/subfiles
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old new 1 *.aux 2 *.bbl 3 *.blg 4 *.fdb* 5 *.fls 6 *.idx 7 *.ilg 1 8 *.ind 2 *.ilg 9 *.lo* 10 *.out 11 *.pdf 12 *.pyg 13 *.tdo 14 *.toc 15 *.xdv 16 cache*
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NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/doc/latex/NEMO/subfiles/chap_model_basics.tex
r11693 r14789 5 5 \chapter{Model Basics} 6 6 \label{chap:MB} 7 8 \thispagestyle{plain}9 7 10 8 \chaptertoc … … 706 704 In this case, the free surface equation is nonlinear, 707 705 and the variations of volume are fully taken into account. 708 These coordinates systems is presented in a report \citep{levier.treguier.ea_ rpt07} available on706 These coordinates systems is presented in a report \citep{levier.treguier.ea_trpt07} available on 709 707 the \NEMO\ web site. 710 708 … … 841 839 This problem can be at least partially overcome by mixing $s$-coordinate and 842 840 step-like representation of bottom topography 843 \citep{gerdes_JGR93 *a,gerdes_JGR93*b,madec.delecluse.ea_JPO96}.841 \citep{gerdes_JGR93,gerdes_JGR93*a,madec.delecluse.ea_JPO96}. 844 842 However, the definition of the model domain vertical coordinate becomes then a non-trivial thing for 845 843 a realistic bottom topography:
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