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Changes between Version 293 and Version 294 of doc/app/runtime_parameters


Ignore:
Timestamp:
Nov 12, 2018 4:48:06 PM (7 years ago)
Author:
gronemeier
Comment:

--

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  • doc/app/runtime_parameters

    v293 v294  
    9090||='''Quantity name''' =||='''Meaning''' =||='''Unit''' =||='''Remarks''' =||
    9191||e  ||SGS turbulence kinetic energy||m^2^/s^2^ || ||
    92 ||thetal ||liquid water potential temperature ||K ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.''||
    9392||lwp* ||liquid water path ||kg/m^2^ ||only horizontal cross section is allowed, requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.'' ||
    9493||nr ||rain drop number density ||1/m^3^ ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.'' and [[../inipar#cloud_scheme|cloud_scheme]] = ''seifert_beheng'' and [[../inipar#precipitation|precipitation]] = ''.T.''||
    … …  
    10099||prr* ||precipitation rate ||mm/s ||only horizontal cross section is allowed, requires [[../inipar#cloud_scheme|cloud_scheme]] = ''kessler'' and [[../inipar#precipitation|precipitation]] = ''.T.'' ||
    101100||prr ||precipitation rate ||kg/kg m/s ||requires [[../inipar#cloud_scheme|cloud_scheme]] = ''seifert_beheng'' and [[../inipar#precipitation|precipitation]] = ''.T.''||
    102 ||theta ||potential temperature ||K || ||
    103101||q ||water vapor mixing ratio (or total water mixing ratio if cloud physics is switched on) ||kg/kg ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    104102||qc ||cloud water mixing ratio ||kg/kg ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.'' and [[../inipar#cloud_scheme|cloud_scheme]] = ''seifert_beheng'' ||
    … …  
    116114||ssws* ||surface scalarflux ||kg m^-2^ s^-1^ or ppm m s^-1^ ||only horizontal cross section is allowed (see [[#section_xy|section_xy]]), requires [[../inipar#passive_scalar|passive_scalar]] = ''.T.'' ||
    117115||t* ||(near surface) characteristic temperature ||K ||only horizontal cross section is allowed ||
     116||theta ||potential temperature ||K || ||
     117||thetal ||liquid water potential temperature ||K ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.''||
     118||thetav ||virtual potential temperature ||K ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
     119||tsurf* ||surface temperature ||K ||only horizontal cross section is allowed ||
    118120||u ||u-component of the velocity ||m/s || ||
    119121||us* ||(near surface) friction velocity ||m/s ||only horizontal cross section is allowed ||
    120122||v ||v-component of the velocity ||m/s || ||
    121 ||thetav ||virtual potential temperature ||K ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    122123||w ||w-component of the velocity ||m/s || ||
    123124||z0* ||roughness length ||m || ||
    124125||z0h* ||roughness length for scalar quantities ||m || ||
    125 ||tsurf* ||surface temperature ||K ||only horizontal cross section is allowed ||
    126126\\
    127127The following quantities can be additionally output when the [wiki:doc/tec/lsm land surface model (LSM)] is used:
    … …  
    200200||='''Quantity name''' =||='''Meaning''' =||='''Unit''' =||='''Remarks''' =||
    201201||e  ||SGS turbulence kinetic energy|| m^2^/s^2^ || ||
    202 ||thetal ||liquid water potential temperature ||K ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.''||
    203202||nr ||rain drop number density ||1/m^3^ ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.'' and [[../inipar#cloud_scheme|cloud_scheme]] = ''seifert_beheng'' and [[../inipar#precipitation|precipitation]] = ''.T.''||
    204203||p ||perturpation pressure ||N/m^2^, Pa || ||
    205204||pc ||particle/droplet concentration ||#/gridbox || ||
    206205||pr ||mean particle/droplet radius ||m || ||
    207 ||theta ||potential temperature ||K || ||
    208206||q ||water vapor mixing ratio (or total water mixing ratio if cloud physics is switched on) ||kg/kg ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    209207||qc ||cloud water mixing ratio ||kg/kg ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.'' and [[../inipar#cloud_scheme|cloud_scheme]] = ''seifert_beheng'' ||
    … …  
    217215||s ||concentration of the scalar ||kg m^-3^ or ppm ||requires [[../inipar#passive_scalar|passive_scalar]] = ''.T.'' ||
    218216||sa ||salinity ||psu ||requires [[../inipar#ocean|ocean]] = ''.T.'' ||
     217||theta ||potential temperature ||K || ||
     218||thetal ||liquid water potential temperature ||K ||requires [[../inipar#cloud_physics|cloud_physics]] = ''.T.''||
     219||thetav ||virtual potential temperature ||K ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    219220||u ||u-component of the velocity ||m/s || ||
    220221||v ||v-component of the velocity ||m/s || ||
    221 ||thetav ||virtual potential temperature ||K ||requires [[../inipar#humidity|humidity]] = ''.T.'' ||
    222222||w ||w-component of the velocity ||m/s || ||
    223223'''Example:'''
    … …  
    256256The following list shows the values which can be assigned to '''data_output_pr'''. The profile data is either defined on u-v-levels (variables marked in [[span(red,style=color: red)]]) or on w-levels ([[span(green,style=color: green)]]). According to this, the z-coordinates of the individual profiles vary. Beyond that, with a constant flux layer switched on ([[../inipar#constant_flux_layer|constant_flux_layer]]) the lowest output level is z = zu(1) instead of z = zw(0) for profiles w"u", w"v", wu and wv. Turbulence quantities such as w*u* or u*2 are calculated from turbulent fluctuations that are defined as deviations from the instantaneous horizontal average.\\\\
    257257||='''Quantity name''' =||='''Meaning''' =||='''Unit''' =||
     258||[[span(e ,style=color: red)]] ||Turbulence kinetic energy (TKE, subgrid-scale) ||m^2^/s^2^ ||
     259||[[span(e* ,style=color: red)]] ||Perturbation energy (resolved) (composed of variances or fluxes, see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
     260||[[span(hyp ,style=color: red)]] ||Hydrostatic Pressure ||hPa ||
     261||[[span(hyp ,style=color: red)]] ||Hydrostatic pressure ||dbar ||
     262||[[span(kh ,style=color: red)]] ||Eddy diffusivity for heat ||m^2^/s ||
     263||[[span(km ,style=color: red)]] ||Eddy diffusivity for momentum ||m^2^/s ||
     264||[[span(l ,style=color: red)]] ||Mixing length ||m ||
     265||[[span(nr ,style=color: red)]] ||Rain drop number density ||1/m^3^ ||
     266||[[span(p ,style=color: red)]] ||Perturbation pressure ||Pa ||
     267||[[span(prho ,style=color: red)]] ||Potential density ||kg/m^3^ ||
     268||[[span(q ,style=color: red)]] ||Total water mixing ratio ||kg/kg ||
     269||[[span(q*2 ,style=color: red)]] ||Variance of the water vapor / total water mixing ratio (in case of  [../inipar#cloud_physics cloud_physics] = .T.) (resolved) ||kg^2^/kg^2^ ||
     270||[[span(qc ,style=color: red)]] ||Cloud water mixing ratio ||kg/kg ||
     271||[[span(ql ,style=color: red)]] ||Liquid water mixing ratio ||kg/kg ||
     272||[[span(qr ,style=color: red)]] ||Rain water mixing ratio ||kg/kg ||
     273||[[span(qv ,style=color: red)]] ||Water vapor mixing ratio ||kg/kg ||
     274||[[span(prr ,style=color: red)]] ||Precipitation rate ||kg/kg m/s||
     275||[[span(rho ,style=color: red)]] ||Air Density ||kg/m^3^ ||
     276||[[span(rho_sea_water ,style=color: red)]] ||Ocean Density ||kg/m^3^ ||
     277||[[span(s ,style=color: red)]] ||Scalar concentration (requires [[../inipar#passive_scalar|passive_scalar]] = ''.T.'')  ||kg m^-3^ or ppm ||
     278||[[span(s*2 ,style=color: red)]] ||Variance of the passive scalar (resolved, requires [../inipar#passive_scalar passive_scalar] = .T.) ||(kg m^-3^)^2^ ||
     279||[[span(sa ,style=color: red)]] ||Salinity ||psu ||
     280||[[span(Sw ,style=color: green)]] ||Skewness of the w-velocity component (resolved, Sw = w^3^/(w^2^)^1.5^) ||m^3^/s^2^ / (m^2^/s^2^)^1.5^ ||
     281||[[span(td_lsa_q ,style=color: red)]] ||horizontal large scale advection tendency for humidity||kg/(kg s) ||
     282||[[span(td_lsa_thetal ,style=color: red)]] ||horizontal large scale advection tendency for temperature||K/s ||
     283||[[span(td_nud_q ,style=color: red)]] ||nudging tendency for humidity||kg/(kg s) ||
     284||[[span(td_nud_thetal ,style=color: red)]] ||nudging tendency for temperature||K/s ||
     285||[[span(td_nud_u ,style=color: red)]] ||nudging tendency for u-velocity component||m/s^2^ ||
     286||[[span(td_nud_v ,style=color: red)]] ||nudging tendency for v-velocity component||m/s^2^ ||
     287||[[span(td_sub_q ,style=color: red)]] ||horizontal large scale subsidence tendency for humidity||kg/(kg s) ||
     288||[[span(td_sub_thetal ,style=color: red)]] ||horizontal large scale subsidence tendency for temperature||K/s ||
     289||[[span(theta ,style=color: red)]] ||Potential temperature ||K ||
     290||[[span(theta*2 ,style=color: red)]] ||Variance of the potential temperature (resolved) ||K^2^ ||
     291||[[span(thetal ,style=color: red)]] ||Liquid water potential temperature ||K ||
     292||[[span(thetav ,style=color: red)]] ||Virtual potential temperature ||K ||
    258293||[[span(u ,style=color: red)]] ||u-component of the velocity ||m/s ||
     294||[[span(u*2 ,style=color: red)]] ||Variance or horizontal momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the u-velocity component (resolved) ||m^2^/s^2^ ||
     295||[[span(ug ,style=color: red)]] ||u-component of the geostrophic wind ||m/s ||
    259296||[[span(v ,style=color: red)]] ||v-component of the velocity ||m/s ||
    260 ||[[span(ug ,style=color: red)]] ||u-component of the geostrophic wind ||m/s ||
     297||[[span(v*2 ,style=color: red)]] ||Variance or horizontal momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the v-velocity component (resolved) ||m^2^/s^2^ ||
    261298||[[span(vg ,style=color: red)]] ||v-component of the geostrophic wind ||m/s ||
    262299||[[span(w ,style=color: green)]] ||w-component of the velocity ||m/s ||
    263 ||[[span(w_subs ,style=color: red)]] ||large-scale vertical velocity ||m/s ||
    264 ||[[span(theta ,style=color: red)]] ||Potential temperature ||K ||
    265 ||[[span(thetav ,style=color: red)]] ||Virtual potential temperature ||K ||
    266 ||[[span(thetal ,style=color: red)]] ||Liquid water potential temperature ||K ||
    267 ||[[span(q ,style=color: red)]] ||Total water mixing ratio ||kg/kg ||
    268 ||[[span(qv ,style=color: red)]] ||Water vapor mixing ratio ||kg/kg ||
    269 ||[[span(ql ,style=color: red)]] ||Liquid water mixing ratio ||kg/kg ||
    270 ||[[span(hyp ,style=color: red)]] ||Hydrostatic Pressure ||hPa ||
    271 ||[[span(rho ,style=color: red)]] ||Air Density ||kg/m^3^ ||
    272 ||[[span(rho_sea_water ,style=color: red)]] ||Ocean Density ||kg/m^3^ ||
    273 ||[[span(prho ,style=color: red)]] ||Potential density ||kg/m^3^ ||
    274 ||[[span(s ,style=color: red)]] ||Scalar concentration (requires [[../inipar#passive_scalar|passive_scalar]] = ''.T.'')  ||kg m^-3^ or ppm ||
    275 ||[[span(sa ,style=color: red)]] ||Salinity ||psu ||
    276 ||[[span(e ,style=color: red)]] ||Turbulence kinetic energy (TKE, subgrid-scale) ||m^2^/s^2^ ||
    277 ||[[span(e* ,style=color: red)]] ||Perturbation energy (resolved) (composed of variances or fluxes, see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
    278 ||[[span(p ,style=color: red)]] ||Perturbation pressure ||Pa ||
    279 ||[[span(km ,style=color: red)]] ||Eddy diffusivity for momentum ||m^2^/s ||
    280 ||[[span(kh ,style=color: red)]] ||Eddy diffusivity for heat ||m^2^/s ||
    281 ||[[span(l ,style=color: red)]] ||Mixing length ||m ||
    282 ||[[span(nr ,style=color: red)]] ||Rain drop number density ||1/m^3^ ||
    283 ||[[span(qc ,style=color: red)]] ||Cloud water mixing ratio ||kg/kg ||
    284 ||[[span(qr ,style=color: red)]] ||Rain water mixing ratio ||kg/kg ||
    285 ||[[span(prr ,style=color: red)]] ||Precipitation rate ||kg/kg m/s||
    286 ||[[span(w"u" ,style=color: green)]] ||u-component of the subgrid-scale vertical momentum flux ||m^2^/s^2^ ||
    287 ||[[span(w*u* ,style=color: green)]] ||Covariance or u-component of the resolved vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
    288 ||[[span(wu ,style=color: green)]] ||u-component of the total vertical momentum flux (w"u" + w*u*) ||m^2^/s^2^ ||
    289 ||[[span(w"v" ,style=color: green)]] ||v-component of the subgrid-scale vertical momentum flux ||m^2^/s^2^ ||
    290 ||[[span(w*v* ,style=color: green)]] ||Covariance or v-component of the resolved vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
    291 ||[[span(wv ,style=color: green)]] ||v-component of the total vertical momentum flux (w"v" + w*v*) ||m^2^/s^2^ ||
    292 ||[[span(w"theta" ,style=color: green)]] ||Subgrid-scale vertical sensible heat flux ||K m/s ||
    293 ||[[span(w*theta* ,style=color: green)]] ||Covariance or resolved vertical sensible heat flux (in case of [../inipar#scalar_advec scalar_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||K m/s ||
    294 ||[[span(wtheta ,style=color: green)]] ||Total vertical sensible heat flux (w"theta" + w*theta*) ||K m/s ||
    295 ||[[span(w*theta*BC ,style=color: green)]] ||Subgrid-scale vertical sensible heat flux using the Bott-Chlond scheme ||K m/s ||
    296 ||[[span(wthetaBC ,style=color: green)]] ||Total vertical sensible heat flux using the Bott-Chlond scheme (w"theta" + w*theta*BC) ||K m/s ||
    297 ||[[span(w"thetav" ,style=color: green)]] ||Subgrid-scale vertical buoyancy flux ||K m/s ||
    298 ||[[span(w*thetav* ,style=color: green)]] ||Resolved vertical buoyancy flux ||K m/s ||
    299 ||[[span(wthetav ,style=color: green)]] ||Total vertical buoyancy flux (w"thetav" + w*thetav*) ||K m/s ||
     300||[[span(w*2 ,style=color: green)]] ||Variance or vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the w-velocity component (resolved) ||m^2^/s^2^ ||
     301||[[span(w*3 ,style=color: green)]] ||Third moment of the w-velocity component (resolved) ||m^3^/s^3^ ||
     302||[[span(w*e* ,style=color: green)]] ||Vertical flux of perturbation energy (resolved) ||m^3^/s^3^ ||
     303||[[span(w*p*:dz ,style=color: red)]] ||Transport of resolved-scale TKE due to pressure fluctuations (term in resolved TKE budget)||Pa m/s^2^ ||
    300304||[[span(w"q" ,style=color: green)]] ||Subgrid-scale vertical water flux ||kg/kg m/s ||
    301305||[[span(w*q* ,style=color: green)]] ||Covariance or resolved vertical water flux (in case of [../inipar#scalar_advec scalar_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||kg/kg m/s ||
    … …  
    310314||[[span(w*sa* ,style=color: green)]] ||Covariance or resolved vertical salinity flux (in case of [../inipar#scalar_advec scalar_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||psu m/s ||
    311315||[[span(wsa  ,style=color: green)]] ||Total vertical salinity flux (w"sa" + w*sa*) ||psu m/s ||
    312 ||[[span(w*e* ,style=color: green)]] ||Vertical flux of perturbation energy (resolved) ||m^3^/s^3^ ||
    313 ||[[span(u*2 ,style=color: red)]] ||Variance or horizontal momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the u-velocity component (resolved) ||m^2^/s^2^ ||
    314 ||[[span(v*2 ,style=color: red)]] ||Variance or horizontal momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the v-velocity component (resolved) ||m^2^/s^2^ ||
    315 ||[[span(w*2 ,style=color: green)]] ||Variance or vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) of the w-velocity component (resolved) ||m^2^/s^2^ ||
    316 ||[[span(theta*2 ,style=color: red)]] ||Variance of the potential temperature (resolved) ||K^2^ ||
    317 ||[[span(q*2 ,style=color: red)]] ||Variance of the water vapor / total water mixing ratio (in case of  [../inipar#cloud_physics cloud_physics] = .T.) (resolved) ||kg^2^/kg^2^ ||
    318 ||[[span(s*2 ,style=color: red)]] ||Variance of the passive scalar (resolved, requires [../inipar#passive_scalar passive_scalar] = .T.) ||(kg m^-3^)^2^ ||
    319 ||[[span(w*3 ,style=color: green)]] ||Third moment of the w-velocity component (resolved) ||m^3^/s^3^ ||
    320 ||[[span(Sw ,style=color: green)]] ||Skewness of the w-velocity component (resolved, Sw = w^3^/(w^2^)^1.5^) ||m^3^/s^2^ / (m^2^/s^2^)^1.5^ ||
     316||[[span(w_subs ,style=color: red)]] ||large-scale vertical velocity ||m/s ||
     317||[[span(w"theta" ,style=color: green)]] ||Subgrid-scale vertical sensible heat flux ||K m/s ||
     318||[[span(w*theta* ,style=color: green)]] ||Covariance or resolved vertical sensible heat flux (in case of [../inipar#scalar_advec scalar_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||K m/s ||
     319||[[span(wtheta ,style=color: green)]] ||Total vertical sensible heat flux (w"theta" + w*theta*) ||K m/s ||
     320||[[span(w*theta*BC ,style=color: green)]] ||Subgrid-scale vertical sensible heat flux using the Bott-Chlond scheme ||K m/s ||
     321||[[span(wthetaBC ,style=color: green)]] ||Total vertical sensible heat flux using the Bott-Chlond scheme (w"theta" + w*theta*BC) ||K m/s ||
     322||[[span(w"thetav" ,style=color: green)]] ||Subgrid-scale vertical buoyancy flux ||K m/s ||
     323||[[span(w*thetav* ,style=color: green)]] ||Resolved vertical buoyancy flux ||K m/s ||
     324||[[span(wthetav ,style=color: green)]] ||Total vertical buoyancy flux (w"thetav" + w*thetav*) ||K m/s ||
    321325||[[span(w*2theta* ,style=color: green)]] ||Third moment (resolved) ||K m^2^/s^2^ ||
    322326||[[span(w*theta*2 ,style=color: green)]] ||Third moment (resolved) ||K^2^ m/s ||
     327||[[span(w"u" ,style=color: green)]] ||u-component of the subgrid-scale vertical momentum flux ||m^2^/s^2^ ||
     328||[[span(w*u* ,style=color: green)]] ||Covariance or u-component of the resolved vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
     329||[[span(wu ,style=color: green)]] ||u-component of the total vertical momentum flux (w"u" + w*u*) ||m^2^/s^2^ ||
    323330||[[span(w*u*u*:dz ,style=color: red)]] ||Transport of resolved-scale TKE due to turbulence (term in resolved TKE budget)||m^2^/s^3^ ||
    324 ||[[span(w*p*:dz ,style=color: red)]] ||Transport of resolved-scale TKE due to pressure fluctuations (term in resolved TKE budget)||Pa m/s^2^ ||
    325 ||[[span(hyp ,style=color: red)]] ||Hydrostatic pressure ||dbar ||
    326 ||[[span(td_lsa_thetal ,style=color: red)]] ||horizontal large scale advection tendency for temperature||K/s ||
    327 ||[[span(td_lsa_q ,style=color: red)]] ||horizontal large scale advection tendency for humidity||kg/(kg s) ||
    328 ||[[span(td_sub_thetal ,style=color: red)]] ||horizontal large scale subsidence tendency for temperature||K/s ||
    329 ||[[span(td_sub_q ,style=color: red)]] ||horizontal large scale subsidence tendency for humidity||kg/(kg s) ||
    330 ||[[span(td_nud_thetal ,style=color: red)]] ||nudging tendency for temperature||K/s ||
    331 ||[[span(td_nud_q ,style=color: red)]] ||nudging tendency for humidity||kg/(kg s) ||
    332 ||[[span(td_nud_u ,style=color: red)]] ||nudging tendency for u-velocity component||m/s^2^ ||
    333 ||[[span(td_nud_v ,style=color: red)]] ||nudging tendency for v-velocity component||m/s^2^ ||
     331||[[span(w"v" ,style=color: green)]] ||v-component of the subgrid-scale vertical momentum flux ||m^2^/s^2^ ||
     332||[[span(w*v* ,style=color: green)]] ||Covariance or v-component of the resolved vertical momentum flux (in case of [../inipar#momentum_advec momentum_advec] = 'ws-scheme', see [../../tec/advection#statistical_evaluation details]) ||m^2^/s^2^ ||
     333||[[span(wv ,style=color: green)]] ||v-component of the total vertical momentum flux (w"v" + w*v*) ||m^2^/s^2^ ||
    334334\\
    335335The following vertical profiles can be additionally output when the [wiki:doc/tec/lsm land surface model (LSM)] is used:
    … …  
    534534The file contains the following time-series quantities (the first column gives the name of the quantities as used in the NetCDF file), all of which are automatically output without having to be prescribed by the user, since the size of the time-series file is rather small:\\\\
    535535||='''Quantity name''' =||='''Meaning''' =||='''Unit''' =||
     536||div_new ||Divergence of the velocity field after the pressure solver has been called (normalized with respect to the total number of grid points) ||1/s ||
     537||div_old ||Divergence of the velocity field before the pressure solver has been called (normalized with respect to the total number of grid points) ||1/s ||
     538||dt ||Time step size ||s ||
    536539||E ||Total kinetic energy of the flow, E = 0.5 * (u^2^+v^2^+w^2^), (3D domain average) ||m^2^/s^2^ ||
    537540||E* ||Resolved-scale turbulence kinetic energy of the flow (3D domain average) ||m^2^/s^2^ ||
    538 ||dt ||Time step size ||s ||
     541||ol ||Monin-Obukhov length ||m ||
     542||q* ||Humidity scale (constant flux layer), defined as w"q"0 / us* (horizontal average)||kg/kg ||
     543||th* ||Temperature scale (constant flux layer), defined as w"theta"0 / us* (horizontal average)||K ||
     544||theta(0) ||Potential temperature at the surface (horizontal average) ||K ||
     545||theta(z_mo) ||Potential temperature for z = zu(1) (horizontal average) ||K ||
     546||umax ||Maximum u-component of the velocity ||m/s ||
    539547||us* ||Friction velocity (horizontal average) ||m/s ||
     548||vmax ||Maximum v-component of the velocity ||m/s ||
    540549||w* ||Vertical velocity scale of the CBL (horizontal average) ||m/s ||
    541 ||th* ||Temperature scale (constant flux layer), defined as w"theta"0 / us* (horizontal average)||K ||
    542 ||q* ||Humidity scale (constant flux layer), defined as w"q"0 / us* (horizontal average)||kg/kg ||
    543 ||umax ||Maximum u-component of the velocity ||m/s ||
    544 ||vmax ||Maximum v-component of the velocity ||m/s ||
    545 ||wmax ||Maximum w-component of the velocity ||m/s ||
    546 ||div_old ||Divergence of the velocity field before the pressure solver has been called (normalized with respect to the total number of grid points) ||1/s ||
    547 ||div_new ||Divergence of the velocity field after the pressure solver has been called (normalized with respect to the total number of grid points) ||1/s ||
    548 ||zi_wtheta ||Height of the convective boundary layer (horizontal average) determined by the height of the minimum sensible heat flux ||m ||
    549 ||zi_theta ||Height of the convective boundary layer (horizontal average) determined by the temperature profile, following the criterion of Sullivan et al. (1998) ||m ||
     550||w"q"0 ||Subgrid-scale humidity flux at k=0 (horizontal average) within the constant flux layer, zero values are output if humidity is not used ||kg/kg m/s ||
     551||w"theta" ||Subgrid-scale heat flux (horizontal average) for z = zw(1) ||K m/s ||
    550552||w"theta"0 ||Subgrid-scale sensible heat flux at k=0 (horizontal average) within the constant flux layer ||K m/s ||
    551 ||w"theta" ||Subgrid-scale heat flux (horizontal average) for z = zw(1) ||K m/s ||
    552 ||wtheta ||Total heat flux (horizontal average) for z = zw(1) ||K m/s ||
    553553||w"u"0 ||Subgrid-scale momentum flux (u-component) at k=0 (horizontal average) within the constant flux layer||m^2^/s^2^ ||
    554554||w"v"0 ||Subgrid-scale momentum flux (v-component) at k=0 (horizontal average) within the constant flux layer ||m^2^/s^2^ ||
    555 ||w"q"0 ||Subgrid-scale humidity flux at k=0 (horizontal average) within the constant flux layer, zero values are output if humidity is not used ||kg/kg m/s ||
    556 ||theta(0) ||Potential temperature at the surface (horizontal average) ||K ||
    557 ||theta(z_mo) ||Potential temperature for z = zu(1) (horizontal average) ||K ||
    558 ||ol ||Monin-Obukhov length ||m ||
     555||wmax ||Maximum w-component of the velocity ||m/s ||
     556||wtheta ||Total heat flux (horizontal average) for z = zw(1) ||K m/s ||
     557||zi_theta ||Height of the convective boundary layer (horizontal average) determined by the temperature profile, following the criterion of Sullivan et al. (1998) ||m ||
     558||zi_wtheta ||Height of the convective boundary layer (horizontal average) determined by the height of the minimum sensible heat flux ||m ||
    559559\\
    560560The following quantities are additionally output when the [wiki:doc/tec/lsm land surface model (LSM)] is used:
                                                                                                                                                                                                                                                                                                                                                                               
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