ZETA_SETUP

 &meso  
   dt     = 120.	; time step for this segment [sec]  
   mstart = 1	  	; starting time index (set to 1 for 1st segment)
   mend   = 1000   	; ending time index  
   mcn    = 1000		; frequency of restart writes [timesteps]  
   mhn    = 200		; frequency of history writes [timesteps]  
   cfil   = 0.05	; Robert (Asselin) filter coefficient  
   ht     = 18.e+3	; height of rigid lid [m]
   epsi   = 0.1		; geometric scale factor in vertical coordinate transformation 
   rlonmin = -30.0	; longitude of western boundary mass point [deg] -180. < rlonmin < rlonmax < 180.
   rlonmax =  30.0	; longitude of eastern boundary mass point [deg] -180. < rlonmin < rlonmax < 180.
   rlatmin = 42.5	; latitude of south wall [deg] -90. < rlatmin < rlatmax < 90.
   rlatmax = 47.5	; latitude of north wall [deg] -90. < rlatmin < rlatmax < 90.
   shear  = 0.e-3       ; vertical shear in basic state zonal wind [/sec]  
   bvfsq  = 1.0e-4	; Brunt-Vaisala frequency squared of tropospheric basic state [/sec**2] 
   tho    = 300.        ; potential temperature at the ground [K]  
   thy    = 0.0         ; unused  
   rkh    = 5.0e+4	; horizontal diffusion coefficient [m**2/sec]  
   rkv    = 20.		; vertical   diffusion coefficient [m**2/sec]  
   fnorm  = 4.5         ; unused  
   rkh4   = 0.00        ; fourth-order horizontal diffusion coefficient [m**4/sec]  
 &end  
 &mesomnt  
   hmnt   = 1000.	; maximum mountain height [m]  
   efwx   = 50.e+3	; mountain e-folding width in zonal direction [m]  
   efwy   = 100.e+3	; mountain e-folding width in merid direction [m]  
   ywid   = 5000.e+3	; width of constant-height plateau in merid direction [m]  
   imnt   =  0. 	; longitude of mountain peak [deg]
   jmnt   = 45.		; latitude of mountain peak [deg]
   angle  = 0.		; clockwise rotation angle of mountain [degrees]  
 &end  
 &mesoinit  
   U0       = 20.0	; surface wind [m/sec] 
   eadyamp  = 0.0	; amplitude of initial Eady wave [mb] 
   rsshramp  = 0.0	; amplitude of Rossby-Haurwitz wave [m/sec] 
   lread    = F         ; read in initial condition? 
   lmntint  = F         ; interpolate fields back to heights without topography? 
   masscont = F         ; apply mass continuity over topography initially? 
   jetset   = F         ; set a jet structure for the basic flow? 
   jetbeg   = 20.	; latitude of jet beginning [deg]
   jetend   = 70.	; latitude of jet end [deg]
   KSTRATOS  = 99       ; z-index of tropopause 
   KINTERF   = 99       ; z-index of shear change 
 &end  
 &tropopause  
   trpmid = 14.e+3	; height of tropopause at middle of jet [m]
   trpamp = 2.0e+3	; amplitude of tropopause variation at middle of jet [m]
   trpyscldeg = 7.	; y-scale of the tropopause variation [degrees] 
   uvscl = 3.0e+3 	; vertical scale of u-variation [m] (d(Cor)/dzee ~ tanh((z-ztrop)/uvscl))
 &end  
 &mesobc  
   ispwid   = 11	; width of sponge in zonal direction [index units] (0 => no sponge)
   jspwid   = 0		; width of polar sponge [index units] (0 => no sponge)
   bndwrit  = F         ; write out zonal boundaries for subsequent input? 
   bndread  = F         ; read in zonal boundary conditions? 
 &end  
 &mesovmix
  rnumin = 0.1		; minimum value of viscosity coefficient [m**2/sec]
  rnumax = 10.0		; maximum value of viscosity coefficient [m**2/sec]
  richcrit = 2.0	; critical Richardson number where rnuv=0.5(rnuvmax+rnuvmin)
  delrich = 2.0		; half-width of richardson number transition zone
 &end  
 &mesovort  
   vortamp = 0.0e-4     ; amplitude of initial barotropic vortex [/s] 
   vefwx   = 2000.e+3    ; e-folding width in x of barotropic vortex [m] 
   vefwy   = 2000.e+3    ; e-folding width in x of barotropic vortex [m] 
   ivort   = 15         ; x-index of barotropic vortex center 
   jvort   = 34         ; y-index of barotropic vortex center 
 &end  
 &upforc  
   upvamp  = 1.0        ; amplitude of upstream meridional velocity (Eady wave) forcing [m/s] 
   upvper  = 100000.    ; period of upstream meridional velocity forcing [s]
 &end  
 &densprof  
   rho0  = 1.0		; density at the ground [kg/m**3] 
   h_rho_inv = 1.	; anelastic switch (0 => Bousinesq, 1 => anelastic)
 &end  
 &tracepnt  
   ITRACE  = 370	; x-index of trace point
   JTRACE  = 97		; y-index of trace point
   KTRACE  = 3		; z-index of trace point
 &end  
 &mesotraj  
   mtn  = 0		; timesteps between subdomain writes 
   ixtb = 49		; x-index of western subdomain boundary 
   ixte = 97		; x-index of eastern subdomain boundary 
   iytb = 56		; y-index of southern subdomain boundary 
   iyte = 168		; y-index of northern subdomain boundary 
   iztb = 1		; z-index of bottom of subdomain boundary 
   izte = 15		; z-index of top of subdomain boundary 
 &end  
 &sclzonp 
   mszp  = 0		; time between renormalizations [sec] (0 => no renormalization)
   pamp = 0.01		; max zonal pert. amp of v after renormalization [m/sec]
 &end