Changeset 11676
- Timestamp:
- 2019-10-11T00:15:24+02:00 (5 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_ZDF.tex
r11675 r11676 574 574 of the pycnocline (the stratified region at the bottom of the OSBL). 575 575 576 Presently, mixing below the OSBL is handled by the Richardson 577 number-dependent mixing scheme used in \citet{large.ea_RG97}. 578 579 Convective parameterizations such as described in \ref{sec:ZDF_conv} 580 below should not be used with the OSMOSIS-OBL model: instabilities 581 within the OSBL are part of the model, while instabilities below the 582 ML are handled by the Ri # dependent scheme. 583 584 \subsubsection{The structure of the OSBL} 585 Figure \ref{OSM1} 576 586 577 587 \subsubsection{The flux gradient model}
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