6.9. jules_vegetation.nml
¶
This file sets the vegetation options. It contains one namelist called JULES_VEGETATION
.
HCTN24 refers to Hadley Centre Technical Note 24, available from the Met Office Library.
6.9.1. JULES_VEGETATION
namelist members¶
-
JULES_VEGETATION::
l_trait_phys
¶ Type: logical Default: F Switch for using trait-based physiology.
- TRUE
- Vcmax is calculated based on observed leaf traits. Leaf nitrogen (nmass: kgN kgLeaf-1) and leaf mass (LMA: kgLeaf m-2) can be based on observations from the TRY database. Vcmax (umol CO2 m-2 s-1) is based on linear regressions as in Kattge et al. 2009. Two additional parameters are needed: vint and vsl - the intercept and slope, respectively, that relate the leaf nitrogen to vcmax. Sigl is replaced with LMA (sigl=LMA*Cmass, where Cmass is the kgC/kgLeaf and is 0.4).
- FALSE
- Vcmax is calculated based on parameters nl0 (kgN kgC-1) and neff.
-
JULES_VEGETATION::
l_phenol
¶ Type: logical Default: F Switch for vegetation phenology model.
- TRUE
- Use phenology model.
- FALSE
- Do not use phenology model.
-
JULES_VEGETATION::
l_triffid
¶ Type: logical Default: F Switch for dynamic vegetation model (TRIFFID) except for competition.
- TRUE
- Use TRIFFID. In this case soil carbon is modelled using four pools (biomass, humus, decomposable plant material, resistant plant material).
- FALSE
- Do not use TRIFFID. A single soil carbon pool is used.
-
JULES_VEGETATION::
l_veg_compete
¶ Type: logical Default: T Switch for competing vegetation.
Only used if
l_triffid
= TRUE.- TRUE
- TRIFFID will let the different PFTs compete against each other and modify the vegetation fractions.
- FALSE
- Vegetation fractions do not change.
-
JULES_VEGETATION::
l_ht_compete
¶ Type: logical Default: F Only used if
l_triffid
= TRUE.- TRUE
Use height-based vegetation competition (recommended).
This allows for a generic number of PFTs. When
l_trif_eq
= TRUE, this is implemented bylotka_eq_jls.F90
. Whenl_trif_eq
= FALSE, it is implemented inlotka_noeq_jls.F90
whenl_trif_crop
= FALSE and inlotka_noeq_subset_jls.F90
whenl_trif_crop
= TRUE.- FALSE
Use the vegetation competition described in HCTN24.
This is hard-wired for 5 PFTs (BT, NT, C3, C4, SH, in that order) with co-competition for grasses and trees in
lokta_jls.F90
.
-
JULES_VEGETATION::
l_nitrogen
¶ Type: logical Default: F Only used if
l_triffid
= TRUE.- TRUE
- Enable Nitrogen limitation of carbon uptake. A nitrogen deposition field should be provided otherwise no N deposition is assumed.
- FALSE
- No Nitrogen limitation. Nitrogen fluxes are calculated as diagnostics only.
-
JULES_VEGETATION::
l_trif_eq
¶ Type: logical Default: T Switch for equilibrium vegetation model (i.e., an equilibrium solution of TRIFFID).
Only used if
l_triffid
= TRUE.- TRUE
- Use equilibrium TRIFFID.
- FALSE
- Do not use equilibrium TRIFFID.
-
JULES_VEGETATION::
phenol_period
¶ Type: integer Permitted: >= 1 Default: None Period for calls to phenology model in days. Only relevant if
l_phenol
= TRUE.
-
JULES_VEGETATION::
triffid_period
¶ Type: integer Permitted: >= 1 Default: None Period for calls to TRIFFID model in days. Only relevant if one of
l_triffid
orl_trif_eq
is TRUE.
-
JULES_VEGETATION::
l_gleaf_fix
¶ Type: logical Default: T Switch for fixing a bug in the accumulation of
g_leaf_phen_acc
.This bug occurs because
veg2
is called on TRIFFID timesteps andveg1
is called on phenol timesteps, butveg1
did not previously accumulateg_leaf_phen_acc
in the same way asveg2
.- TRUE
veg1
accumulatesg_leaf_phen_acc
between calls to TRIFFID. This is important iftriffid_period
>phenol_period
.- FALSE
veg1
does not accumulateg_leaf_phen_acc
between calls to TRIFFID.
-
JULES_VEGETATION::
l_bvoc_emis
¶ Type: logical Default: F Switch to enable calculation of BVOC emissions.
- TRUE
- BVOC emissions diagnostics will be calculated.
- FALSE
- BVOC emissions diagnostics will not be calculated.
-
JULES_VEGETATION::
l_o3_damage
¶ Type: logical Default: F Switch for ozone damage.
- TRUE
Ozone damage is on.
Note
Ozone concentration in ppb must be prescribed in prescribed_data.nml.
- FALSE
- No effect.
-
JULES_VEGETATION::
l_stem_resp_fix
¶ Type: logical Default: F Switch for bug fix for stem respiration to use balanced LAI to derive respiring stem mass. The switch is included for backwards compatability with existing configurations. Future updates should include this change.
- TRUE
- Respiring stem mass is derived allometrically.
- FALSE
- Respiring stem mass varies with seasonal LAI
-
JULES_VEGETATION::
l_scale_resp_pm
¶ Type: logical Default: F Scale whole plant maintanence respiration by the soil moisture stress factor, instead of only scaling leaf respiration.
- TRUE
- Soil moisture stress reduces leaf, root, and stem maintanence respiration.
- FALSE
- Soil moisture stress only reduces leaf maintanence respiration.
-
JULES_VEGETATION::
fsmc_shape
¶ Type: integer Permitted: 0,1 Default: 0 Shape of soil moisture stress function on vegetation (fsmc).
- Piece-wise linear in vol. soil moisture.
- Piece-wise linear in soil potential. Currently only allowed when
const_z
= T andl_use_pft_psi
= T.
Note
The option
fsmc_shape
= 1 is still in development. Users should ensure that results are as expected, and provide feedback where deficiencies are identified.
-
JULES_VEGETATION::
l_use_pft_psi
¶ Type: logical Default: F Switch for parameters in the soil moisture stress on vegetation function (fsmc).
- TRUE
- Fsmc is calculated from
psi_close_io
andpsi_open_io
. - FALSE
- Fsmc is calculated from
sm_wilt
andsm_crit
inJULES_SOIL_PROPS
andfsmc_p0_io
.
Note
Soil respiration and surface conductance of bare soil respectively will depend on
sm_wilt
andsm_crit
inJULES_SOIL_PROPS
, regardless of the setting offsmc_shape
.Note
The option
l_use_pft_psi
= T is still in development. Users should ensure that results are as expected, and provide feedback where deficiencies are identified.
-
JULES_VEGETATION::
l_vegcan_soilfx
¶ Type: logical Default: F Switch for enhancement to canopy model to allow for conduction in the soil below the vegetative canopy, reducing coupling between the soil and the canopy.
- TRUE
- Allow for conduction in the soil.
- FALSE
- No effect.
-
JULES_VEGETATION::
l_leaf_n_resp_fix
¶ Type: logical Default: F Switch for bug fix for leaf nitrogen content used in the calculation of plant maintenance respiration. The switch is included for backwards compatability with existing configurations. Runs with
can_rad_mod
=1, 4 or 5 are affected.- TRUE
- Use correct forms for canopy-average leaf N content.
- FALSE
- No effect.
-
JULES_VEGETATION::
l_landuse
¶ Type: logical Default: F Switch for using landuse change in conjunction with TRIFFID
Only used if
l_triffid
= TRUE.- TRUE
- Land use change is implemented within TRIFFID. Litter fluxes are split between soil and wood product pools. Requires additional prognostics covering the product pools and the agricultural fraction from the previous TRIFFID call.
- FALSE
- All litter fluxes enter the soil
-
JULES_VEGETATION::
l_recon
¶ Type: logical Default: T Switch for reconfiguring vegetation fractions. Also initialises vegetation and soil biogeochemistry at land ice points. With the ECOSSE soil model this switch also ensures that the initial condition for soil biogeochemistry is internally consistent.
- TRUE
- For soil points (land points with no ice) ensure vegetation fractions are at least a minimum value and reduce other fractions accordingly.
- FALSE
- Do not apply the minimum vegation fractions. This is useful when some points are 100% lake and urban, in which case reconfiguration leads to a total tile fraction of greater than 1.
-
JULES_VEGETATION::
l_prescsow
¶ Type: logical Default: F Switch that determines how crop sowing dates are defined. Only used if
ncpft
> 0.- TRUE
- Sowing dates prescribed in
JULES_CROP_PROPS
are used. - FALSE
- Sowing dates are determined by the model.
-
JULES_VEGETATION::
l_irrig_dmd
¶ Type: logical Default: F Switch controlling the implementation of irrigation demand code.
- TRUE
- Tiles are irrigated.
- FALSE
- No effect.
-
JULES_VEGETATION::
l_irrig_limit
¶ Type: logical Default: F Switch controlling whether the amount of water used to irrigate tiles is limited.
- TRUE
Water for irrigation is taken first from the deep soil (groundwater) store, and then from the river storage when the deep soil store is exhausted. Tiles are irrigated up to the critical point if the necessary water is available. This option requires
l_irrig_dmd
= TRUE,l_top
= TRUE,l_rivers
= TRUE andi_river_vn
=1,3
.Warning
The irrigation supply code in JULES is still in development, and is available in this release to support beta testing activities.
Users should ensure that results are as expected, and provide feedback where deficiencies are identified.
- FALSE
- Tiles will be irrigated to critical point from an unconstrained water supply.
-
JULES_VEGETATION::
l_trif_crop
¶ Type: logical Default: F Switch controlling the treatment of agricultural PFTs. Where agricultural PFTs are defined by the
crop_io
parameter.- TRUE
- In the non-agricultural area natural PFT competion is calculated by a call to a new version of the lotka routine and in each agricultural area agricultural-PFT competition is calculated by an additional call to the new version of the lotka routine. Crop and pasture areas are defined by the
frac_agr
andfrac_past
variables respectively. Additionally, to represent harvesting, a fraction of crop litter is added to the fast wood products pool instead of the soil carbon pools. - FALSE
- Vegetation competition is calculated for natural and crop PFTs together, with natural PFTs excluded from the agricultural area that is defined by the
frac_agr
variable. Agricultural PFTs can also grow in natural areas where they are interpreted as natural grasses.
-
JULES_VEGETATION::
irr_crop
¶ Type: integer Permitted: 0, 1 or 2 Default: 0 - Irrigation season (i.e. season in which crops might be growing on the gridbox) lasts the entire year.
- Irrigation season is determined from driving data according to Doell & Siebert (2002) method. No irrigation is applied outside the irrigation season.
- Irrigation season is determined by maximum dvi across all tiles. Requires l_crop = T. No irrigation is applied outside the irrigation season.
-
JULES_VEGETATION::
can_model
¶ Type: integer Permitted: 1-4 Default: 4 Choice of canopy model for vegetation:
- No distinct canopy.
- Radiative canopy with no heat capacity.
- Radiative canopy with heat capacity. This option is deprecated, with 4 preferred.
- As 3 but with a representation of snow beneath the canopy. This option is preferred to 3.
Note
can_model
= 1 does not mean that there is no vegetation canopy. It means that the surface is represented as a single entity, rather than having distinct surface and canopy levels for the purposes of radiative processes.
-
JULES_VEGETATION::
can_rad_mod
¶ Type: integer Permitted: 1, 4, 5, 6 Default: 4 Switch for treatment of canopy radiation.
- A single canopy layer for which radiation absorption is calculated using Beer’s law. Leaf-level photosynthesis is scaled to the canopy level using the ‘big leaf’ approach. Leaf nitrogen, photosynthetic capacity, i.e the Vcmax parameter, and leaf photosynthesis vary exponentially through the canopy with radiation.
- Multi-layer approach for radiation interception following the 2-stream approach of Sellers et al. (1992). This approach takes into account leaf angle distribution, zenith angle, and differentiates absorption of direct and diffuse radiation. It has an exponential decline of leaf N through the canopy and includes inhibition of leaf respiration in the light. Canopy photosynthesis and conductance are calculated as the sum over all layers.
- This is an improvement of option 4, including:
- Sunfleck penetration though the canopy.
- Division of sunlit and shaded leaves within each canopy level.
- A modified version of inhibition of leaf respiration in the light.
- This is an improvement of option 5, including an exponential decline of leaf N with canopy height proportional to LAI, following Beer’s law.
Note
can_rad_mod
= 1 and 6 are recommended.Note
When using
can_rad_mod
= 4, 5 or 6 it is recommended to use driving data that contains direct and diffuse radiation separately rather than a constant diffuse fraction.See also
Descriptions of option 1 can be found in Jogireddy et al. (2006), and an application of option 4 can be found in Mercado et al. (2007). Options 1 to 5 are described in Clark et al (2011).
-
JULES_VEGETATION::
ilayers
¶ Type: integer Permitted: >= 0 Default: 10 Number of layers for canopy radiation model. Only used for
can_rad_mod
= 4, 5 or 6.These layers are used for the calculations of radiation interception and photosynthesis.
-
JULES_VEGETATION::
stomata_model
¶ Type: integer Permitted: 1 or 2 Default: 1 Choice for model of stomatal conductance.
Possible values are:
- The original JULES model, including the Jacobs closure - see Eqn.9 of Best et al. (2011).
- The model of Medlyn et al. (2011) - see Eqn.11 of that paper, and Medlyn et al (2012). Note that as implemented the model uses a single parameter (g1, assuming that g0 = 0).
See also
References:
- Best et al., 2011, The Joint UK Land Environment Simulator (JULES), model description – Part 1: Energy and water fluxes, Geosci. Model Dev., https://doi.org/10.5194/gmd-4-677-2011.
- Medlyn et al., 2011, Reconciling the optimal and empirical approaches to modelling stomatal conductance, Global Change Biology, https://doi.org/10.1111/j.1365-2486.2010.02375.x.
- Medlyn et al., 2012, Reconciling the optimal and empirical approaches to modelling stomatal conductance, Global Change Biology, https://doi.org/10.1111/j.1365-2486.2012.02790.x.
-
JULES_VEGETATION::
frac_min
¶ Type: real Default: 1.0e-6 Minimum fraction that a PFT is allowed to cover if TRIFFID is used.
-
JULES_VEGETATION::
frac_seed
¶ Type: real Default: 0.01 Seed fraction for TRIFFID.
-
JULES_VEGETATION::
pow
¶ Type: real Default: 5.241e-4 Power in sigmodial function used to get competition coefficients.
See Hadley Centre Technical Note 24, Eq.3.
-
JULES_VEGETATION::
l_inferno
¶ Type: logical Default: F Switch that determines whether interactive fires (INFERNO) is used. This allows for the diagnostic of burnt area, burnt carbon and a variety of fire emissions.
- TRUE
- INFERNO is used to provide diagnostic fire variables
- FALSE
- INFERNO is not used.
-
JULES_VEGETATION::
ignition_method
¶ Type: integer Permitted: 1, 2, 3 Default: 1 Switch to determine the type of ignition used (ubiquitous or prescribed with population and lightning)
- INFERNO uses ubiquitous (constant) ignitions, of 1.67 fires per km2 per s (1.5 from humans, 0.17 from lightning).
- INFERNO uses prescribed lightning ignitions, either from an ancillary or the UM. Meanwhile humans are assumed to ignite 1.5 fires per km2 per s.
- INFERNO uses prescribed ignition using Population Density and Lightning Frequency (Cloud-to-Ground). These must be provided as prescribed data to the JULES run.
-
JULES_VEGETATION::
l_trif_fire
¶ Type: logical Default: F Switch that determines whether interactive fire is used. This allows for burnt area to link with dynamic vegetation.
Only used if
l_triffid
= TRUE.- TRUE
- Burnt area is calculated in INFERNO and passed to TRIFFID to calculate vegetation dynamics. Carbon is also removed from DPM and RPM pools in SOILCARB.
- FALSE
- Burnt area is zero unless prescribed via an ancillary file.
-
JULES_VEGETATION::
l_vegdrag_pft
¶ Type: logical(npft) Default: F Switch for using vegetation canopy drag scheme on each PFT.
- TRUE
- Use a vegetative drag scheme. This is based on Harman and Finnigan (2007).
- FALSE
- Do not use vegetative drag scheme.
-
JULES_VEGETATION::
l_rsl_scalar
¶ Type: logical Default: F Switch for using a roughness sublayer correction scheme in scalar variables. This is based on Harman and Finnigan (2008).
Only use if any l_vegdrag_pft = TRUE.
- TRUE
- Use a roughness sublayer correction scheme in scalar variables.
- FALSE
- Do not use a roughness sublayer correction scheme in scalar variables.
-
JULES_VEGETATION::
c1_usuh
¶ Type: real Permitted: >= 0 Default: None u*/U(h) at the top of dense canopy. See Massman (1997).
Only use if any l_vegdrag_pft = TRUE.
-
JULES_VEGETATION::
c2_usuh
¶ Type: real Permitted: >= 0 Default: None u*/U(h) at substrate under canopy. See Massman (1997).
Only use if any l_vegdrag_pft = TRUE.
-
JULES_VEGETATION::
c3_usuh
¶ Type: real Permitted: >= 0 Default: None This is used in the exponent of eqution weighting dense and sparse vegetation to get u*/U(h) in neutral condition. See Massman (1997). The default value is taken from Wang (2012).
Only use if any l_vegdrag_pft = TRUE.
-
JULES_VEGETATION::
cd_leaf
¶ Type: real Permitted: 0:1 Default: None Leaf level drag coefficient.
Only use if any l_vegdrag_pft = TRUE.
-
JULES_VEGETATION::
stanton_leaf
¶ Type: real Permitted: 0:1 Default: None Leaf-level Stanton number
Only use if l_rsl_scalar = TRUE.
-
JULES_VEGETATION::
l_spec_veg_z0
¶ Type: logical Default: F Switch for using specified values of the vegetation roughness length rather than being determined by the canopy height.
- TRUE
- Vegetation roughness lengths are specified in z0v_io
- FALSE
- Vegetation roughenss lengths are calculated using canopy heights and parameter dz0v_dh_io.
-
JULES_VEGETATION::
l_limit_canhc
¶ Type: logical Default: F Switch for limiting the canopy heat capacity for vegetation, which is calculated from the canopy height.
Using the SIMARD canopy height ancillary gives very large heat capacities in the Amazon, so this switch limits the areal heat calacity to 1.15e5 J Kg-1 m-2, which is the value calculated by the default broadleaf tree height of 19.01 m..
- TRUE
- Vegetation areal heat capacity limited.
- FALSE
- Vegetation areal heat capacity unlimited.