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- 2020-12-04T20:15:58+01:00 (3 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_model_basics.tex
r11693 r14113 706 706 In this case, the free surface equation is nonlinear, 707 707 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 on708 These coordinates systems is presented in a report \citep{levier.treguier.ea_trpt07} available on 709 709 the \NEMO\ web site. 710 710 … … 841 841 This problem can be at least partially overcome by mixing $s$-coordinate and 842 842 step-like representation of bottom topography 843 \citep{gerdes_JGR93 *a,gerdes_JGR93*b,madec.delecluse.ea_JPO96}.843 \citep{gerdes_JGR93,gerdes_JGR93*a,madec.delecluse.ea_JPO96}. 844 844 However, the definition of the model domain vertical coordinate becomes then a non-trivial thing for 845 845 a realistic bottom topography:
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