6.13. jules_deposition.nml
¶
This file contains options and parameters for modelling of dry deposition of atmospheric trace constituents. It contains a variable number of namelists depending on the required model configuration. The namelist JULES_DEPOSITION
is always required, and one or more instances of the namelist JULES_DEPOSITION_SPECIES
is required if dry deposition has been selected.
Warning
Atmospheric deposition in JULES is still in development and is far from fully functional in this version - the code is included to allow further development. Users should not try to activate the deposition code: leave l_deposition
as FALSE.
6.13.1. JULES_DEPOSITION
namelist members¶
-
JULES_DEPOSITION::
l_deposition
¶ Type: logical Default: FALSE Switch to activate deposition code in JULES.
- TRUE
- Model deposition in JULES.
- FALSE
- Do not model deposition in JULES.
Only used if l_deposition
= TRUE.
-
JULES_DEPOSITION::
dry_dep_model
¶ Type: integer Permitted: 1 Default: none Choice for model of dry deposition.
Possible values are:
- Parameterisation based on that found in UKCA (but now implemented in JULES).
-
JULES_DEPOSITION::
l_deposition_flux
¶ Type: logical Default: FALSE Switch for calculation of deposition fluxes as opposed to deposition velocities.
- TRUE
- Calculate deposition fluxes. This requires that the concentrations of atmopsheric tracer species are provided as prescribed data (see List of supported variables).
- FALSE
- Calculate deposition velocities.
Only used if l_deposition
= TRUE and dry_dep_model
= 1 (UKCA).
-
JULES_DEPOSITION::
ndry_dep_species
¶ Type: integer Permitted: >= 1 Default: none Number of species for which dry deposition is calculated.
-
JULES_DEPOSITION::
l_ukca_ddep_lev1
¶ Type: logical Default: FALSE Switch controlling which atmospheric levels are used for dry deposition.
- TRUE
- Deposition occurs only from the lowest atmospheric level.
- FALSE
- Deposition occurs from all levels within the atmospheric boundary layer.
-
JULES_DEPOSITION::
tundra_s_limit
¶ Type: real Default: none Latitude of southern limit of tundra (degrees). This is used to alter the calculation of deposition of certain species in the tundra region (actually for all points north of this limit). Only used if the list of species (see
dep_species_name_io
) includes one or more of ‘CO’, ‘NO2’, ‘O3’, ‘PAN’, ‘PPAN’, ‘MPAN’ or ‘ONITU’.
-
JULES_DEPOSITION::
dzl_const
¶ Type: real Default: none Constant value for separation of boundary layer levels (m). All layer thicknesses are set to this value. This is used as a simple way to prescribe the layer thicknesses in standalone mode. This value can be overriden by prescribed data - see
JULES_PRESCRIBED
. This can be considered as the representative depth for tracer concentration and the depth over which the deposition flux is removed.
6.13.2. Notes on the JULES_DEPOSITION
namelist¶
The height of the atmospheric boundary layer is required and is set to a default constant value of 1000 m. This value can be overridden via the namelist variable bl_height
, or can be prescribed (i.e. allowed to vary in time and/or space) by providing bl_height
as prescribed data (see List of supported variables).
The number of model levels in the boundary layer is required and is set to a default balues of 1. This can be overridden via the namelist variable bl_levels
. The number of levels is only used to communicate with the atmospheric model (e.g. UKCA).
The separation of the model levels in the boundary layer is required and is set to a constant value via dzl_const
. The separation can be prescribed (i.e. allowed to vary in time and/or space) by providing level_separation
as prescribed data (see List of supported variables). This can be considered as the representative depth for tracer concentration and the depth over which the deposition flux is removed.
If deposition fluxes (rather than deposition velocities) are to be calculated (see l_deposition_flux
), the concentrations of atmospheric tracer species need to be prescribed (see tracer_field
in List of supported variables).
6.13.3. JULES_DEPOSITION_SPECIES
namelist members¶
This namelist should occur ndry_dep_species
times, with each occurence containing parameters for an atmospheric tracer species that is to be considered in dry deposition.
-
JULES_DEPOSITION_SPECIES::
dep_species_name_io
¶ Type: character Default: none Name of an atmospheric tracer species to be included in deposition modelling.
-
JULES_DEPOSITION_SPECIES::
diffusion_coeff_io
¶ Type: real Default: none Diffusion coefficient (m-2 s-1).
-
JULES_DEPOSITION_SPECIES::
rsurf_std_io
¶ Type: real(ntype) Default: none Standard value of surface resistance for each surface type (s m-1).
Only used if dep_species_name_io
= NO2
, O3
, PAN
, PPAN
, MPAN
or ONITU
. Values provided for other species will be ignored.
-
JULES_DEPOSITION_SPECIES::
diffusion_corr_io
¶ Type: real Default: none Diffusion correction factor for stomatal resistance, accounting for the different diffusivities of water and other species (dimensionless).
Only used if dep_species_name_io
= CO
, NO2
, O3
, PAN
, PPAN
, MPAN
or ONITU
. Values provided for other species will be ignored.
-
JULES_DEPOSITION_SPECIES::
r_tundra_io
¶ Type: real Default: none Surface resistance used in tundra region (s m-1).
Only used if dep_species_name_io
= CH4
.
-
JULES_DEPOSITION_SPECIES::
ch4_scaling_io
¶ Type: real Default: none Scaling applied to methane soil uptake (dimensionless). (Originally this was used to match the value from the IPCC Third Assessment Report.)
-
JULES_DEPOSITION_SPECIES::
ch4dd_tundra_io
¶ Type: real(4) Default: none Coefficients of cubic polynomial relating methane loss for tundra to temperature. Flux is in units of ug (CH4) m-2 s-1.
Only used if dep_species_name_io
= H2
.
-
JULES_DEPOSITION_SPECIES::
h2dd_c_io
¶ Type: real(ntype) Default: none Constant in quadratic function relating hydrogen deposition to soil moisture (s m-1).
-
JULES_DEPOSITION_SPECIES::
h2dd_m_io
¶ Type: real(ntype) Default: none Coefficient of first order term in quadratic function relating hydrogen deposition to soil moisture (s m-1).
-
JULES_DEPOSITION_SPECIES::
h2dd_q_io
¶ Type: real(ntype) Default: none Coefficient of second order term in quadratic function relating hydrogen deposition to soil moisture (s m-1).
Only used if dep_species_name_io
= HNO3
, HONO2
or ISON
.
-
JULES_DEPOSITION_SPECIES::
dd_ice_coeff
¶ Type: real(3) Default: none Coefficients in quadratic function relating dry deposition over ice to temperature.
Only used if dep_species_name_io
= O3
.
-
JULES_DEPOSITION_SPECIES::
cuticle_o3_io
¶ Type: real Default: none Constant for calculation of cuticular resistance for ozone (s m-1).
-
JULES_DEPOSITION_SPECIES::
r_wet_soil_o3_io
¶ Type: real Default: none Wet soil surface resistance for ozone (s m-1).