- Timestamp:
- 2011-10-25T15:39:07+02:00 (13 years ago)
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branches/2011/dev_r2855_INGV2_3_blk_wave/DOC/TexFiles/Chapters/Chap_SBC.tex
r2541 r2990 24 24 \end{itemize} 25 25 26 F ourdifferent ways to provide the first six fields to the ocean are available which26 Five different ways to provide the first six fields to the ocean are available which 27 27 are controlled by namelist variables: an analytical formulation (\np{ln\_ana}~=~true), 28 28 a flux formulation (\np{ln\_flx}~=~true), a bulk formulae formulation (CORE 29 (\np{ln\_core}~=~true) or CLIO (\np{ln\_clio}~=~true) bulk formulae) and a coupled 29 (\np{ln\_core}~=~true), CLIO (\np{ln\_clio}~=~true) or MFS 30 \footnote { Note that MFS bulk formulae compute fluxes only for the ocean component} 31 (\np{ln\_ecmwf}~=~true) bulk formulae) and a coupled 30 32 formulation (exchanges with a atmospheric model via the OASIS coupler) 31 33 (\np{ln\_cpl}~=~true). When used, the atmospheric pressure forces both 32 ocean and ice dynamics (\np{ln\_apr\_dyn}~=~true) 33 \footnote{The surface pressure field could be use in bulk formulae, nevertheless 34 none of the current bulk formulea (CLIO and CORE) uses the it.}. 34 ocean and ice dynamics (\np{ln\_apr\_dyn}~=~true). 35 35 The frequency at which the six or seven fields have to be updated is the \np{nn\_fsbc} 36 36 namelist parameter. … … 46 46 (\np{nn\_ice}~=~0,1, 2 or 3); the addition of river runoffs as surface freshwater 47 47 fluxes or lateral inflow (\np{ln\_rnf}~=~true); the addition of a freshwater flux adjustment 48 in order to avoid a mean sea-level drift (\np{nn\_fwb}~=~0,~1~or~2); andthe48 in order to avoid a mean sea-level drift (\np{nn\_fwb}~=~0,~1~or~2); the 49 49 transformation of the solar radiation (if provided as daily mean) into a diurnal 50 cycle (\np{ln\_dm2dc}~=~true). 50 cycle (\np{ln\_dm2dc}~=~true); and a neutral drag coefficient can be read from an external wave 51 model(\np{ln\_cdgw}~=~true). The latter option is possible only in case core or ecmwf bulk formulas are selected. 51 52 52 53 In this chapter, we first discuss where the surface boundary condition appears in the 53 model equations. Then we present the f ourways of providing the surface boundary condition,54 model equations. Then we present the five ways of providing the surface boundary condition, 54 55 followed by the description of the atmospheric pressure and the river runoff. 55 56 Next the scheme for interpolation on the fly is described. … … 480 481 % Bulk formulation 481 482 % ================================================================ 482 \section [Bulk formulation (\textit{sbcblk\_core} or \textit{sbcblk\_clio}) ]483 {Bulk formulation \small{(\mdl{sbcblk\_core} or \mdl{sbcblk\_clio} module)} }483 \section [Bulk formulation (\textit{sbcblk\_core}, \textit{sbcblk\_clio} or \textit{sbcblk\_ecmwf}) ] 484 {Bulk formulation \small{(\mdl{sbcblk\_core} \mdl{sbcblk\_clio} \mdl{sbcblk\_ecmwf} modules)} } 484 485 \label{SBC_blk} 485 486 … … 487 488 using bulk formulae and atmospheric fields and ocean (and ice) variables. 488 489 489 The atmospheric fields used depend on the bulk formulae used. T wobulk formulations490 are available : the CORE and CLIObulk formulea. The choice is made by setting to true491 one of the following namelist variable : \np{ln\_core} and \np{ln\_clio}.492 493 Note : in forced mode, when a sea-ice model is used, a bulk formulation have to be used.494 Therefore the two bulk formulea providedinclude the computation of the fluxes over both490 The atmospheric fields used depend on the bulk formulae used. Three bulk formulations 491 are available : the CORE, the CLIO and the MFS bulk formulea. The choice is made by setting to true 492 one of the following namelist variable : \np{ln\_core} ; \np{ln\_clio} or \np{ln\_ecmwf}. 493 494 Note : in forced mode, when a sea-ice model is used, a bulk formulation (CLIO or CORE) have to be used. 495 Therefore the two bulk (CLIO and CORE) formulea include the computation of the fluxes over both 495 496 an ocean and an ice surface. 496 497 … … 583 584 namelist (see \S\ref{SBC_fldread}). 584 585 586 % ------------------------------------------------------------------------------------------------------------- 587 % ECMWF Bulk formulea 588 % ------------------------------------------------------------------------------------------------------------- 589 \subsection [MFS Bulk formulea (\np{ln\_ecmwf}=true)] 590 {MFS Bulk formulea (\np{ln\_ecmwf}=true, \mdl{sbcblk\_ecmwf})} 591 \label{SBC_blk_ecmwf} 592 %------------------------------------------namsbc_ecmwf---------------------------------------------------- 593 \namdisplay{namsbc_ecmwf} 594 %---------------------------------------------------------------------------------------------------------- 595 596 The MFS (Mediterranean Forecasting System) bulk formulae have been developed by 597 \citet{Castellari_al_JMS1998}. 598 They have been designed to handle the ECMWF operational data and are currently 599 in use in the MFS operational system \citep{Tonani_al_OS08}, \citep{Oddo_al_OS09}. 600 The wind stress computation uses a drag coefficient computed according to \citet{Hellerman_Rosenstein_JPO83}. 601 The surface boundary condition for temperature involves the balance between surface solar radiation, 602 net long-wave radiation, the latent and sensible heat fluxes. 603 Solar radiation is dependent on cloud cover and is computed by means of 604 an astronomical formula \citep{Reed_JPO77}. Albedo monthly values are from \citet{Payne_JAS72} 605 as means of the values at $40^{o}N$ and $30^{o}N$ for the Atlantic Ocean (hence the same latitudinal 606 band of the Mediterranean Sea). The net long-wave radiation flux 607 \citep{Bignami_al_JGR95} is a function of 608 air temperature, sea-surface temperature, cloud cover and relative humidity. 609 Sensible heat and latent heat fluxes are computed by classical 610 bulk formulae parameterized according to \citet{Kondo1975}. 611 Details on the bulk formulae used can be found in \citet{Maggiore_al_PCE98} and \citet{Castellari_al_JMS1998}. 612 613 The required 7 input fields must be provided on the model Grid-T and are: 614 \begin{itemize} 615 \item Zonal Component of the 10m wind ($ms^{-1}$) (\np{sn\_windi}) 616 \item Meridional Component of the 10m wind ($ms^{-1}$) (\np{sn\_windj}) 617 \item Total Claud Cover (\%) (\np{sn\_clc}) 618 \item 2m Air Temperature ($K$) (\np{sn\_tair}) 619 \item 2m Dew Point Temperature ($K$) (\np{sn\_rhm}) 620 \item Total Precipitation ${Kg} m^{-2} s^{-1}$ (\np{sn\_prec}) 621 \item Mean Sea Level Pressure (${Pa}) (\np{sn\_msl}) 622 \end{itemize} 623 % ------------------------------------------------------------------------------------------------------------- 585 624 % ================================================================ 586 625 % Coupled formulation … … 938 977 \end{description} 939 978 979 % ------------------------------------------------------------------------------------------------------------- 980 % Neutral Drag Coefficient from external wave model 981 % ------------------------------------------------------------------------------------------------------------- 982 \subsection [Neutral drag coefficient from external wave model (\textit{sbcwave})] 983 {Neutral drag coefficient from external wave model (\mdl{sbcwave})} 984 \label{SBC_wave} 985 %------------------------------------------namwave---------------------------------------------------- 986 \namdisplay{namsbc_wave} 987 %------------------------------------------------------------------------------------------------------------- 988 \begin{description} 989 If (\np{ln\_cdgw}~=~true) in namsbc namelist is activated the \mdl{sbcwave} module which contains the routine \np{sbc\_wave}.This routine reads the namelist namsbc\_wave and the neutral drag coefficient. Then using the routine TURB\_CORE\_1Z or TURB\_CORE\_2Z the drag coefficient is computed according to stable/unstable conditions of the air-sea interface starting from the neutral drag coefficient. 990 \end{description} 991 940 992 % Griffies doc: 941 993 % When running ocean-ice simulations, we are not explicitly representing land processes, such as rivers, catchment areas, snow accumulation, etc. However, to reduce model drift, it is important to balance the hydrological cycle in ocean-ice models. We thus need to prescribe some form of global normalization to the precipitation minus evaporation plus river runoff. The result of the normalization should be a global integrated zero net water input to the ocean-ice system over a chosen time scale. … … 944 996 945 997 946
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