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- 2016-02-15T16:21:15+01:00 (8 years ago)
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branches/2015/nemo_v3_6_STABLE/DOC/TexFiles/Chapters/Chap_DYN.tex
r6275 r6317 637 637 ($e_{3w}$). 638 638 639 $\bullet$ Traditional coding with adaptation for ice shelf cavities (\np{ln\_hpg\_isf}=true).640 This scheme need the activation of ice shelf cavities (\np{ln\_isfcav}=true).641 642 639 $\bullet$ Pressure Jacobian scheme (prj) (a research paper in preparation) (\np{ln\_dynhpg\_prj}=true) 643 640 … … 654 651 pressure Jacobian method is used to solve the horizontal pressure gradient. This method can provide 655 652 a more accurate calculation of the horizontal pressure gradient than the standard scheme. 653 654 \subsection{Ice shelf cavity} 655 \label{DYN_hpg_isf} 656 Beneath an ice shelf, the total pressure gradient is the sum of the pressure gradient due to the ice shelf load and 657 the pressure gradient due to the ocean load. If cavity opened (\np{ln\_isfcav}~=~true) these 2 terms can be 658 calculated by setting \np{ln\_dynhpg\_isf}~=~true. No other scheme are working with the ice shelf.\\ 659 660 $\bullet$ The main hypothesis to compute the ice shelf load is that the ice shelf is in an isostatic equilibrium. 661 The top pressure is computed integrating from surface to the base of the ice shelf a reference density profile 662 (prescribed as density of a water at 34.4 PSU and -1.9$\degres C$) and corresponds to the water replaced by the ice shelf. 663 This top pressure is constant over time. A detailed description of this method is described in \citet{Losch2008}.\\ 664 665 $\bullet$ The ocean load is computed using the expression \eqref{Eq_dynhpg_sco} described in \ref{DYN_hpg_sco}. 666 A treatment of the partial cell for top and bottom similar to the one described in \ref{DYN_hpg_zps} is done 667 to reduce the residual circulation generated by the top partial cell. 656 668 657 669 %--------------------------------------------------------------------------------------------------------------
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