There are 678 parameters in 15 groups.
| Name | Value | Type | Description |
|---|
gas_constant_dry_air | 287.0 | float | Gas constant for dry air (J kg⁻¹ K⁻¹). |
isobaric_specific_heat_dry_air | 1004.5 | float | Isobaric specific heat of dry air (J kg⁻¹ K⁻¹). |
molar_mass_dry_air | 0.02897 | float | Molar mass of dry air (kg mol⁻¹). |
adiabatic_exponent_dry_air | 0.28571428571 | float | Adiabatic exponent for dry air ($\kappa_d$), derived from $R_d/c_{pd}$ or 2/7 (unitless). |
density_liquid_water | 1000 | float | Density of liquid water (kg m⁻³). |
density_ice_water | 916.7 | float | Density of water ice (kg m⁻³). |
gas_constant_vapor | 461.5 | float | Gas constant for water vapor (J kg⁻¹ K⁻¹). |
molar_mass_water | 0.01801528 | float | Molar mass of water (kg mol⁻¹). |
isobaric_specific_heat_vapor | 1859 | float | Isobaric specific heat of water vapor (J kg⁻¹ K⁻¹). |
isobaric_specific_heat_liquid | 4181 | float | Isobaric specific heat of liquid water (J kg⁻¹ K⁻¹). |
isobaric_specific_heat_ice | 2070.0 | float | Isobaric specific heat of ice (J kg⁻¹ K⁻¹). |
temperature_water_freeze | 273.15 | float | Freezing temperature of water (K). |
temperature_minimum | 150 | float | Minimum temperature for thermodynamic calculations (K). |
specific_humidity_minimum | 1.0e-10 | float | Minimum specific humidity threshold (kg kg⁻¹). Used as a lower bound when comparing or regularizing humidity values. |
specific_humidity_maximum | 0.1 | float | Maximum specific humidity for thermodynamic calculations (kg kg⁻¹). |
temperature_saturation_adjustment_init_min | 150 | float | Minimum temperature for saturation adjustment initialization (K). |
temperature_saturation_adjustment_min | 1 | float | Minimum temperature difference for unsaturated case in saturation adjustment (K). |
temperature_saturation_adjustment_max | 1000 | float | Maximum temperature for saturation adjustment (K). |
temperature_homogenous_nucleation | 233 | float | Temperature for homogeneous ice nucleation (K). |
pow_icenuc | 1 | float | Exponent in the ice nucleation parameterization (unitless). |
temperature_triple_point | 273.16 | float | Triple point temperature of water (K). |
thermodynamics_temperature_reference | 273.16 | float | Reference temperature for thermodynamics (K). |
latent_heat_vaporization_at_reference | 2500800 | float | Latent heat of vaporization at the reference temperature (J kg⁻¹). |
latent_heat_sublimation_at_reference | 2834400 | float | Latent heat of sublimation at the reference temperature (J kg⁻¹). |
pressure_triple_point | 611.657 | float | Triple point pressure of water (Pa). |
surface_tension_water | 0.072 | float | Surface tension of water (N m⁻¹). |
entropy_dry_air | 6864.8 | float | Specific entropy of dry air at the reference temperature and pressure (J kg⁻¹ K⁻¹). |
entropy_water_vapor | 10513.6 | float | Specific entropy of water vapor at the reference temperature and pressure (J kg⁻¹ K⁻¹). |
entropy_reference_temperature | 298.15 | float | Reference temperature for entropy calculations (K). |
potential_temperature_reference_pressure | 100000.0 | float | Reference pressure for potential temperature calculations ($p_0$) (Pa). |
mean_sea_level_pressure | 101325 | float | Mean sea level pressure ($p_{MSL}$) (Pa). |
temperature_surface_reference | 288 | float | Surface temperature in a reference temperature profile (K). |
temperature_min_reference | 215 | float | Minimum temperature in a reference temperature profile (K). |
reference_temperature_exponent | 7 | float | Exponent $s_\text{ref}$ of the Exner function in the hydrostatic reference temperature profile $T_r(p) = T_\text{min} + (T_\text{sfc} - T_\text{min})\,\Pi(p)^{s_\text{ref}}$ (unitless). |
reference_relative_humidity | 0.5 | float | Reference relative humidity used to build a reference total moisture specific humidity profile (unitless). |
reference_moisture_cutoff_pressure | 25000 | float | Pressure cutoff above which the reference-state total-water specific humidity is clipped to zero (Pa). Keeps the reference profile confined to the troposphere, avoiding unphysical stratospheric growth. |
| Name | Value | Type | Description |
|---|
entr_param_vec | [1.0, 1.0, 1.0, …] (12 entries) | float | Data-driven entrainment parameter vector (unitless). |
entr_mult_limiter_coeff | 0.0 | float | Exponent for the multiplicative entrainment limiter of the form $(1 - area)^c$ (unitless). |
turb_entr_param_vec | [0.001, 100000.0, 0.0] | float | Data-driven turbulent entrainment parameter vector (unitless). |
entr_inv_tau | 0 | float | Inverse timescale for entrainment (s⁻¹). |
entr_inv_length | 0 | float | Inverse length scale for entrainment (m⁻¹). |
entr_coeff | 1 | float | Coefficient for the $w/z$ term in the entrainment closure (unitless). |
entr_buoy_coeff | 0 | float | Coefficient for the $b/w^2$ term in the entrainment closure (unitless). |
entr_vertdiv_coeff | 1 | float | Coefficient for the vertical divergence term in the entrainment closure (unitless). |
min_area_limiter_scale | 0.001 | float | Rate coefficient for the minimum area fraction limiter in entrainment (s⁻¹). |
min_area_limiter_power | 1 | float | Exponent for the minimum area fraction limiter in both entrainment and detrainment (unitless). |
entr_detr_limit_inv_tau | 0 | float | Inverse timescale for entrainment and detrainment for negligible area (s⁻¹). |
detr_inv_tau | 0 | float | Inverse timescale for detrainment (s⁻¹). |
detr_coeff | 0.001 | float | Coefficient for the $w$ term in the detrainment closure (unitless). |
detr_buoy_coeff | 0.12 | float | Coefficient for the $b/w^2$ term in the detrainment closure (unitless). Source: Tan et al. (2018), Eq. (27). |
detr_buoy_inv_tau_max | 0.01 | float | Maximum allowed inverse buoyancy timescale (s⁻¹), used to limit detrainment when velocity differences become small and prevent excessively fast detrainment. |
entr_detr_buoy_inv_tau_max | 0.01 | float | Maximum allowed inverse buoyancy timescale (s⁻¹), used to limit entrainment and detrainment when velocity differences become small and prevent excessively fast entrainment and detrainment. |
detr_vertdiv_coeff | 1 | float | Coefficient for the vertical divergence term in the detrainment closure (unitless). |
detr_massflux_vertdiv_coeff | 1 | float | Coefficient for the mass flux vertical divergence term in the detrainment closure (unitless). |
detr_ramp_z_start | 20000.0 | float | Start height of the sigmoid ramp for the detrainment top limiter (m). |
detr_ramp_steepness_factor | 10.0 | float | Factor setting the steepness of the sigmoid ramp for the detrainment top limiter (unitless), where the steepness is the factor divided by $(z_\text{end} - z_\text{start})$. |
max_area_limiter_scale | 0.001 | float | Rate coefficient for the maximum area fraction limiter in detrainment (s⁻¹). |
max_area_limiter_power | 1 | float | Exponent for the maximum area fraction limiter in detrainment (unitless). |
| Name | Value | Type | Description |
|---|
mixing_length_eddy_viscosity_coefficient | 0.14 | float | TKE diffusivity coefficient ($c_m$) for the EDMF mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Table 1. |
mixing_length_diss_coeff | 0.22 | float | TKE dissipation coefficient ($c_d$) for the EDMF mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Table 1. |
mixing_length_static_stab_coeff | 0.4 | float | Static stability coefficient ($c_b$) for the EDMF mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Table 1. |
mixing_length_tke_surf_scale | 3.75 | float | Ratio of TKE to squared friction velocity ($\kappa_*^2$) in the surface layer for the EDMF mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Table 1. |
mixing_length_tke_surf_flux_coeff | 2.5 | float | Coefficient multiplying flux in the $u_*^3$ surface flux formulation of TKE ($C_{flux}$) (unitless). |
mixing_length_Prandtl_number_scale | 4.076923076923077 | float | Cospectral budget factor for turbulent Prandtl number ($\omega_{pr}$) for the EDMF mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Eq. (36). |
mixing_length_Prandtl_number_0 | 0.74 | float | Turbulent Prandtl number in neutral conditions ($Pr_{t,0}$) (unitless). Source: Lopez-Gomez et al. (2020), Table 1. |
mixing_length_Prandtl_maximum | 10 | float | Maximum allowed turbulent Prandtl number (unitless). |
mixing_length_Ri_crit | 0.25 | float | Critical gradient Richardson number ($Ri_{crit}$) (unitless). Source: Li (2019), Section 6.2. |
mixing_length_smin_ub | 0.1 | float | Lower limit for the smooth minimum function in the mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Eq. (40). |
mixing_length_smin_rm | 1.5 | float | Upper ratio limit for the smooth minimum function in the mixing length closure (unitless). Source: Lopez-Gomez et al. (2020), Eq. (40). |
mixing_length_l_max | 1.0e6 | float | Upper limit for the length scale in the mixing length closure (m). Source: Lopez-Gomez et al. (2020). |
mixing_length_l_min | 10 | float | Lower limit for the mixing length (m). |
mixing_length_param_vec | [0.0, 0.0, 0.0, …] (5 entries) | float | Data-driven mixing length parameter vector (unitless). |
| Name | Value | Type | Description |
|---|
microph_scaling_acnv | 1.0 | float | Scaling factor for the 1-moment autoconversion rate (unitless). |
microph_scaling_accr | 1.0 | float | Scaling factor for the 1-moment accretion rate (unitless). |
microph_scaling_evap | 1.0 | float | Scaling factor for the 1-moment rain evaporation rate (unitless). |
microph_scaling_dep_sub | 1.0 | float | Scaling factor for the 1-moment snow deposition/sublimation rate (unitless). |
microph_scaling_melt | 1.0 | float | Scaling factor for the 1-moment snow melting rate (unitless). |
rain_drop_drag_coefficient | 0.55 | float | Rain drop drag coefficient for the 1-moment microphysics scheme (unitless). |
ice_snow_threshold_radius | 6.25e-5 | float | Threshold particle radius separating ice and snow for the 1-moment microphysics scheme (m). |
cloud_ice_size_distribution_coefficient_n0 | 2.0e7 | float | Cloud ice size distribution parameter $n_0$ for the 1-moment microphysics scheme (m⁻⁴). |
cloud_ice_crystals_length_scale | 1.0e-5 | float | Cloud ice particle length scale for the 1-moment microphysics scheme (m). |
cloud_ice_mass_size_relation_coefficient_me | 3 | float | Exponent $m_e$ in the mass-size relation for cloud ice in the 1-moment microphysics scheme (unitless). |
cloud_ice_mass_size_relation_coefficient_chim | 1 | float | Coefficient $\chi_m$ in the mass-size relation for cloud ice in the 1-moment microphysics scheme (unitless). |
cloud_ice_mass_size_relation_coefficient_delm | 0 | float | Coefficient $\delta_m$ in the mass-size relation for cloud ice in the 1-moment microphysics scheme (unitless). |
cloud_liquid_water_specific_humidity_autoconversion_threshold | 0.0005 | float | Rain formation threshold in terms of specific humidity for the 1-moment microphysics scheme (unitless). |
rain_autoconversion_timescale | 1000.0 | float | Rain formation timescale for the 1-moment microphysics scheme (s). Also used as the timescale for strong vertical velocities, when using vertical velocity dependent rain formation. |
rain_autoconversion_timescale_stratiform | 14400 | float | Rain formation timescale for weak vertical velocities when using vertical velocity dependent rain formation (s). |
rain_autoconversion_velocity_scale | 1.5 | float | Blending velocity scale when using vertical velocity dependent rain formation (m s⁻¹). |
rain_ventilation_coefficient_a | 1.5 | float | Rain ventilation coefficient $a$ for the 1-moment microphysics scheme (unitless). |
rain_ventilation_coefficient_b | 0.53 | float | Rain ventilation coefficient $b$ for the 1-moment microphysics scheme (unitless). |
rain_drop_size_distribution_coefficient_n0 | 1.6e7 | float | Rain drop size distribution coefficient $n_0$ for the 1-moment microphysics scheme (m⁻⁴). |
rain_drop_length_scale | 0.001 | float | Rain drop length scale for the 1-moment microphysics scheme (m). |
rain_minimum_inverse_lambda | 1.0e-8 | float | Minimum value for the inverse of the shape parameter $\lambda$ of the rain drop size distribution (m). |
rain_mass_size_relation_coefficient_me | 3 | float | Exponent $m_e$ in the mass-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_cross_section_size_relation_coefficient_ae | 2 | float | Exponent $a_e$ in the cross section-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_terminal_velocity_size_relation_coefficient_ve | 0.5 | float | Exponent $v_e$ in the terminal velocity-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_mass_size_relation_coefficient_chim | 1 | float | Coefficient $\chi_m$ in the mass-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_mass_size_relation_coefficient_delm | 0 | float | Coefficient $\delta_m$ in the mass-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_cross_section_size_relation_coefficient_chia | 1 | float | Coefficient $\chi_a$ in the cross section-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_cross_section_size_relation_coefficient_dela | 0 | float | Coefficient $\delta_a$ in the cross section-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_terminal_velocity_size_relation_coefficient_chiv | 1 | float | Coefficient $\chi_v$ in the terminal velocity-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_terminal_velocity_size_relation_coefficient_delv | 0 | float | Coefficient $\delta_v$ in the terminal velocity-size relation for rain in the 1-moment microphysics scheme (unitless). |
rain_snow_velocity_dispersion_coefficient | 0.2 | float | Velocity dispersion coefficient for rain and snow in the 1-moment microphysics scheme (unitless). |
cloud_liquid_sedimentation_number_concentration | 5.0e8 | float | Number concentration of cloud liquid particles for sedimentation (m⁻³). |
cloud_ice_sedimentation_number_concentration | 5.0e8 | float | Number concentration of cloud ice particles for sedimentation (m⁻³). |
homogeneous_freezing_timescale | 1 | float | Timescale of the homogeneous freezing of cloud liquid droplets into ice (s). |
Reisner_et_al_A_parameter | 0.66 | float | Parameter $A$ for Bigg heterogeneous freezing of cloud droplets (K⁻¹). Source: Reisner et al. (1998), Eq. (A22), DOI: 10.1002/qj.49712454804. |
Reisner_et_al_B_parameter | 100 | float | Parameter $B$ for Bigg heterogeneous freezing of cloud droplets (m⁻³ s⁻¹). Source: Reisner et al. (1998), Eq. (A22), DOI: 10.1002/qj.49712454804. |
cloud_ice_apparent_density | 500 | float | The apparent density of cloud ice particles (kg m⁻³). Source: Lin et al. (2021), DOI: 10.1029/2020JD034157. |
snow_apparent_density | 100 | float | The apparent density of snow particles (kg m⁻³). Source: Lin et al. (2021), DOI: 10.1029/2020JD034157. |
cloud_ice_specific_humidity_autoconversion_threshold | 1.0e-6 | float | Snow autoconversion threshold in terms of specific humidity for the 1-moment microphysics scheme (unitless). |
snow_autoconversion_timescale | 100 | float | Snow autoconversion timescale for the 1-moment microphysics scheme (s). |
snow_ventilation_coefficient_a | 0.65 | float | Snow ventilation coefficient $a$ for the 1-moment microphysics scheme (unitless). |
snow_ventilation_coefficient_b | 0.44 | float | Snow ventilation coefficient $b$ for the 1-moment microphysics scheme (unitless). |
snow_flake_size_distribution_coefficient_mu | 4.36e9 | float | Snow size distribution coefficient $\mu$ for the 1-moment microphysics scheme (m⁻⁴). |
snow_flake_size_distribution_coefficient_nu | 0.63 | float | Snow size distribution coefficient $\nu$ for the 1-moment microphysics scheme (unitless). |
snow_flake_length_scale | 0.001 | float | Snow particle length scale for the 1-moment microphysics scheme (m). |
snow_mass_size_relation_coefficient_me | 2 | float | Exponent $m_e$ in the mass-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_cross_section_size_relation_coefficient | 2 | float | Exponent in the cross section-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_terminal_velocity_size_relation_coefficient | 0.25 | float | Exponent in the terminal velocity-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_mass_size_relation_coefficient_chim | 1 | float | Coefficient $\chi_m$ in the mass-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_mass_size_relation_coefficient_delm | 0 | float | Coefficient $\delta_m$ in the mass-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_cross_section_size_relation_coefficient_chia | 1 | float | Coefficient $\chi_a$ in the cross section-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_cross_section_size_relation_coefficient_dela | 0 | float | Coefficient $\delta_a$ in the cross section-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_terminal_velocity_size_relation_coefficient_chiv | 1 | float | Coefficient $\chi_v$ in the terminal velocity-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_terminal_velocity_size_relation_coefficient_delv | 0 | float | Coefficient $\delta_v$ in the terminal velocity-size relation for snow in the 1-moment microphysics scheme (unitless). |
snow_aspect_ratio | 0.15 | float | Assumed aspect ratio for snow in the 1-moment microphysics scheme (unitless). |
snow_aspect_ratio_coefficient | 0.3333333333333333 | float | Power law coefficient for terminal velocity dependence on snow aspect ratio (unitless). Source: Chen et al. (2022), DOI: 10.1016/j.atmosres.2022.106171. |
cloud_liquid_rain_collision_efficiency | 0.8 | float | Collision efficiency between cloud liquid water and rain for the 1-moment scheme (unitless). |
cloud_liquid_snow_collision_efficiency | 0.1 | float | Collision efficiency between cloud liquid water and snow for the 1-moment scheme (unitless). |
cloud_ice_rain_collision_efficiency | 1 | float | Collision efficiency between cloud ice and rain for the 1-moment scheme (unitless). |
cloud_ice_snow_collision_efficiency | 0.1 | float | Collision efficiency between cloud ice and snow for the 1-moment scheme (unitless). |
rain_snow_collision_efficiency | 1 | float | Collision efficiency between rain and snow for the 1-moment scheme (unitless). |
| Name | Value | Type | Description |
|---|
TC1980_autoconversion_coeff_D | 3268.0 | float | Coefficient $D$ in the Tripoli and Cotton (1980) rain autoconversion parameterization ($m^{3b} s^{-1}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
TC1980_autoconversion_coeff_a | 2.3333333333333335 | float | Coefficient $a$ (default 7/3) in the Tripoli and Cotton (1980) rain autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
TC1980_autoconversion_coeff_b | -0.3333333333333333 | float | Coefficient $b$ (default -1/3) in the Tripoli and Cotton (1980) rain autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
TC1980_autoconversion_coeff_r_0 | 7.0e-6 | float | Threshold size $r_0$ in the Tripoli and Cotton (1980) rain autoconversion parameterization (m). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
TC1980_autoconversion_coeff_me_liq | 3.0 | float | Mass-size relation exponent $m_e$ in the Tripoli and Cotton (1980) scheme (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
TC1980_accretion_coeff_A | 4.7 | float | Coefficient $A$ in the Tripoli and Cotton (1980) accretion parameterization (s⁻¹). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_C | 3.0e34 | float | Coefficient $C$ in the Beheng (1994) autoconversion parameterization ($m^{3(c+b-1)} s^{-1} kg^{-(b-1)}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_a | -1.7 | float | Coefficient $a$ in the Beheng (1994) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_b | 4.7 | float | Coefficient $b$ in the Beheng (1994) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_c | -3.3 | float | Coefficient $c$ in the Beheng (1994) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_d_low | 3.9 | float | Coefficient $d_{low}$ in the Beheng (1994) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_d_high | 9.9 | float | Coefficient $d_{high}$ in the Beheng (1994) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_autoconversion_coeff_N_0 | 2.0e8 | float | Coefficient $N_0$ in the Beheng (1994) autoconversion parameterization (m⁻³). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
B1994_accretion_coeff_A | 6.0 | float | Coefficient $A$ in the Beheng (1994) accretion parameterization (s⁻¹). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_autoconversion_coeff_A | 7.42e13 | float | Coefficient $A$ in the Khairoutdinov and Kogan (2000) autoconversion parameterization ($m^{3(b+c)} s^{-1} kg^{-c}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_autoconversion_coeff_a | 2.47 | float | Coefficient $a$ in the Khairoutdinov and Kogan (2000) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_autoconversion_coeff_b | -1.79 | float | Coefficient $b$ in the Khairoutdinov and Kogan (2000) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_autoconversion_coeff_c | -1.47 | float | Coefficient $c$ in the Khairoutdinov and Kogan (2000) autoconversion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_accretion_coeff_A | 67.0 | float | Coefficient $A$ in the Khairoutdinov and Kogan (2000) accretion parameterization ($m^{3b} kg^{-b} s^{-1}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_accretion_coeff_a | 1.15 | float | Coefficient $a$ in the Khairoutdinov and Kogan (2000) accretion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
KK2000_accretion_coeff_b | -1.3 | float | Coefficient $b$ in the Khairoutdinov and Kogan (2000) accretion parameterization (unitless). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
LD2004_R_6C_coeff | 7.5 | float | Coefficient in the Liu and Daum (2004) autoconversion parameterization ($\mu m^{3/2} kg^{1/6} m^{-1/2}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
LD2004_E_0_coeff | 1.08e10 | float | Coefficient $E_0$ in the Liu and Daum (2004) autoconversion parameterization ($m^3 kg^{-2} s^{-1}$). Source: Wood (2005), DOI: 10.1175/JAS3530.1. |
Variable_time_scale_autoconversion_coeff_alpha | 1.0 | float | Exponent of number density in the function describing the autoconversion timescale (unitless). |
threshold_smooth_transition_steepness | 10.0 | float | Steepness parameter for the smooth transition function used in threshold-based processes (unitless). |
| Name | Value | Type | Description |
|---|
SB2006_collection_kernel_coeff_kcc | 4.44e9 | float | Cloud-cloud collection kernel constant $k_{cc}$ in the Seifert and Beheng (2006) scheme ($m^3 kg^{-2} s^{-1}$). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_collection_kernel_coeff_kcr | 5.25 | float | Cloud-rain collection kernel constant $k_{cr}$ in the Seifert and Beheng (2006) scheme ($m^3 kg^{-1} s^{-1}$). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_collection_kernel_coeff_krr | 7.12 | float | Rain-rain collection kernel constant $k_{rr}$ in the Seifert and Beheng (2006) scheme ($m^3 kg^{-1} s^{-1}$). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_collection_kernel_coeff_kapparr | 60.7 | float | Collection kernel constant $\kappa_{rr}$ in the Seifert and Beheng (2006) scheme ($kg^{-1/3}$). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_cloud_droplets_min_mass | 4.2e-15 | float | Minimum mass of cloud droplets in the Seifert and Beheng (2006) scheme (kg). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_min_mass | 2.6e-10 | float | Minimum mass of raindrops in the Seifert and Beheng (2006) scheme (kg). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_max_mass | 5.0e-6 | float | Maximum mass of raindrops in the Seifert and Beheng (2006) scheme (kg). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_cloud_gamma_distribution_coeff_nu | 1.0 | float | Gamma distribution coefficient $\nu$ for clouds (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_cloud_gamma_distribution_coeff_mu | 1 | float | Gamma distribution coefficient $\mu$ for clouds (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_rain_distribution_coeff_nu | -0.66666666666667 | float | Gamma distribution coefficient $\nu$ for rain (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_rain_distribution_coeff_mu | 0.33333333333333 | float | Gamma distribution coefficient $\mu$ for rain (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_reference_air_density | 1.225 | float | Reference air density at surface conditions (kg m⁻³). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_autoconversion_correcting_function_coeff_A | 400.0 | float | Coefficient $A$ in the universal function correcting the autoconversion rate (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_autoconversion_correcting_function_coeff_a | 0.7 | float | Coefficient $a$ in the universal function correcting the autoconversion rate (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_autoconversion_correcting_function_coeff_b | 3 | float | Coefficient $b$ in the universal function correcting the autoconversion rate (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_accretion_correcting_function_coeff_tau0 | 5.0e-5 | float | Coefficient $\tau_0$ in the universal function correcting the accretion rate (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_accretion_correcting_function_coeff_c | 4 | float | Coefficient $c$ in the universal function correcting the accretion rate (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_self-collection_coeff_d | -5 | float | Coefficient $d$ in the raindrops self-collection rate equation (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_equilibrium_mean_diameter | 0.0009 | float | Equilibrium mean diameter of raindrops for computing the breakup rate (m). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_breakup_mean_diameter_threshold | 0.00035 | float | Threshold of raindrops mean diameter for breakup (m). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_breakup_coeff_kbr | 1000 | float | Coefficient $k_{br}$ in the raindrops breakup rate equation (m⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_breakup_coeff_kappabr | 2300 | float | Coefficient $\kappa_{br}$ in the raindrops breakup rate equation (m⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_terminal_velocity_coeff_aR | 9.65 | float | Coefficient $a_R$ in the raindrops terminal velocity equation (m s⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_terminal_velocity_coeff_bR | 10.3 | float | Coefficient $b_R$ in the raindrops terminal velocity equation (m s⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_terminal_velocity_coeff_cR | 600 | float | Coefficient $c_R$ in the raindrops terminal velocity equation (m⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_ventilation_factor_coeff_av | 0.78 | float | Coefficient $a_v$ in the ventilation factor equation for rain evaporation (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_ventilation_factor_coeff_bv | 0.308 | float | Coefficient $b_v$ in the ventilation factor equation for rain evaporation (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_rain_evaporation_coeff_alpha | 159 | float | Coefficient $\alpha$ in the fallspeed relation for rain evaporation (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_rain_evaporation_coeff_beta | 0.266 | float | Coefficient $\beta$ in the fallspeed relation for rain evaporation (unitless). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_size_distribution_coeff_N0_min | 250000.0 | float | Minimum value of the raindrops size distribution parameter $N_0$ (m⁻⁴). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_size_distribution_coeff_N0_max | 2.0e7 | float | Maximum value of the raindrops size distribution parameter $N_0$ (m⁻⁴). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_size_distribution_coeff_lambda_min | 1000.0 | float | Minimum value of the raindrops size distribution parameter $\lambda$ (m⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
SB2006_raindrops_size_distribution_coeff_lambda_max | 10000.0 | float | Maximum value of the raindrops size distribution parameter $\lambda$ (m⁻¹). Source: Seifert and Beheng (2006), DOI: 10.1007/s00703-005-0112-4. |
Horn2012_number_concentration_adjustment_timescale | 100 | float | Timescale for 2-moment number concentration adjustment (s). Source: Horn (2012), DOI: 10.5194/gmd-5-345-2012. |
| Name | Value | Type | Description |
|---|
Chen2022_table_B1_q_coeff | 0.115231 | float | Coefficient $q$ for raindrop terminal velocity parameterization (unitless). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B1_ai | [0.044612, -0.263166, 4.7178] | float | Coefficients $a_i$ for raindrop terminal velocity parameterization ($mm^{-b_i}$). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B1_a3_pow_coeff | -0.47335 | float | Power coefficient for $a_3$ in raindrop terminal velocity parameterization (unitless). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B1_bi | [2.2955, 2.2955, 1.1451] | float | Coefficients $b_i$ for raindrop terminal velocity parameterization (unitless). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B1_b_rho_coeff | 0.038465 | float | Density coefficient $b_{\rho}$ for raindrop terminal velocity parameterization (m³ kg⁻¹). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B1_ci | [0.0, 0.184325, 0.184325] | float | Coefficients $c_i$ for raindrop terminal velocity parameterization (mm⁻¹). Source: Chen et al. (2022), Table B1, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_As | [-0.263503, 0.00174079, 0.0378769] | float | Coefficients $A_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_Bs | [0.575231, 0.0909307, 0.515579] | float | Coefficients $B_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_Cs | [-0.345387, 0.177362, -0.000427794, 0.00419647] | float | Coefficients $C_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_Es | [-0.156593, 0.0189334, 0.1377817] | float | Coefficients $E_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_Fs | [-3.35641, 0.0156199, 0.765337] | float | Coefficients $F_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B3_Gs | [-0.0309715, 1.55054, 0.518349] | float | Coefficients $G_s$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B3, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Al | [-0.475897, -0.0023127, 1.12293] | float | Coefficients $A_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Bl | [-2.56289, -0.00513504, 0.608459] | float | Coefficients $B_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Cl | [-0.756064, 0.935922, -1.70952] | float | Coefficients $C_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_El | [0.00639847, 0.00906454, -0.108232] | float | Coefficients $E_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Fl | [0.515453, -0.0725042, -1.8681e19] | float | Coefficients $F_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Gl | [2.65236, 0.00158269, 259.935] | float | Coefficients $G_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_table_B5_Hl | [-0.346044, -7.17829e-11, -1.24394e20] | float | Coefficients $H_l$ for ice terminal velocity parameterization. Source: Chen et al. (2022), Table B5, DOI: 10.1016/j.atmosres.2022.106171. |
Chen2022_ice_cutoff | 0.000625 | float | Cutoff diameter between small and large ice particles in the Chen et al. (2022) parameterization (m). Source: Chen et al. (2022), DOI: 10.1016/j.atmosres.2022.106171. |
| Name | Value | Type | Description |
|---|
Mohler2006_maximum_allowed_Si | 1.35 | float | Maximum allowed supersaturation over ice, $S_{i,max}$ (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_threshold_T | 220 | float | Threshold temperature, $T_{thr}$, separating two deposition regimes (K). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_S0_warm_ArizonaTestDust | 1.03 | float | Onset saturation ratio $S_0$ for temperatures > $T_{thr}$ for Arizona Test Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_S0_cold_ArizonaTestDust | 1.07 | float | Onset saturation ratio $S_0$ for temperatures < $T_{thr}$ for Arizona Test Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_a_warm_ArizonaTestDust | 4.7 | float | Coefficient $a$ for temperatures > $T_{thr}$ for Arizona Test Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_a_cold_ArizonaTestDust | 9.2 | float | Coefficient $a$ for temperatures < $T_{thr}$ for Arizona Test Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_S0_warm_DesertDust | 1.17 | float | Onset saturation ratio $S_0$ for temperatures > $T_{thr}$ for Desert Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_S0_cold_DesertDust | 1.03 | float | Onset saturation ratio $S_0$ for temperatures < $T_{thr}$ for Desert Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_a_warm_DesertDust | 0.43 | float | Coefficient $a$ for temperatures > $T_{thr}$ for Desert Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
Mohler2006_a_cold_DesertDust | 2.35 | float | Coefficient $a$ for temperatures < $T_{thr}$ for Desert Dust (unitless). Source: Möhler et al. (2006), DOI: 10.5194/acp-6-3007-2006. |
| Name | Value | Type | Description |
|---|
J_ABDINM_m_Dust | 13.2251 | float | Default empirical coefficient $m$ for the water-activity-based deposition nucleation rate ($J_{het}$) parameterization for dust (unitless). |
J_ABDINM_c_Dust | 0.7716 | float | Default empirical coefficient $c$ for the water-activity-based deposition nucleation rate ($J_{het}$) parameterization for dust (unitless). |
J_ABDINM_m_Illite | 13.2251 | float | Empirical coefficient $m$ for the deposition nucleation rate ($J_{het}$) of Illite (unitless). |
J_ABDINM_c_Illite | 0.7716 | float | Empirical coefficient $c$ for the deposition nucleation rate ($J_{het}$) of Illite (unitless). |
J_ABDINM_m_SaharanDust | 13.2251 | float | Empirical coefficient $m$ for the deposition nucleation rate ($J_{het}$) of Saharan Dust (unitless). |
J_ABDINM_c_SaharanDust | 0.7716 | float | Empirical coefficient $c$ for the deposition nucleation rate ($J_{het}$) of Saharan Dust (unitless). |
J_ABDINM_m_AsianDust | 13.2251 | float | Empirical coefficient $m$ for the deposition nucleation rate ($J_{het}$) of Asian Dust (unitless). |
J_ABDINM_c_AsianDust | 0.7716 | float | Empirical coefficient $c$ for the deposition nucleation rate ($J_{het}$) of Asian Dust (unitless). |
J_ABDINM_m_ArizonaTestDust | 13.2251 | float | Empirical coefficient $m$ for the deposition nucleation rate ($J_{het}$) of Arizona Test Dust (unitless). |
J_ABDINM_c_ArizonaTestDust | 0.7716 | float | Empirical coefficient $c$ for the deposition nucleation rate ($J_{het}$) of Arizona Test Dust (unitless). |
Alpert2022_J_deposition_m_Feldspar | 13.2251 | float | Coefficient $m$ for deposition nucleation rate $J_{het}$ of Feldspar (unitless). Source: Alpert et al. (2022), DOI: 10.1039/D1EA00077B. |
Alpert2022_J_deposition_c_Feldspar | 0.7716 | float | Coefficient $c$ for deposition nucleation rate $J_{het}$ of Feldspar (unitless). Source: Alpert et al. (2022), DOI: 10.1039/D1EA00077B. |
Alpert2022_J_deposition_m_Ferrihydrite | 12.3525 | float | Coefficient $m$ for deposition nucleation rate $J_{het}$ of Ferrihydrite (unitless). Source: Alpert et al. (2022), DOI: 10.1039/D1EA00077B. |
Alpert2022_J_deposition_c_Ferrihydrite | 0.0516 | float | Coefficient $c$ for deposition nucleation rate $J_{het}$ of Ferrihydrite (unitless). Source: Alpert et al. (2022), DOI: 10.1039/D1EA00077B. |
China2017_J_deposition_m_Kaolinite | 27.551 | float | Coefficient $m$ for deposition nucleation rate $J_{het}$ of Kaolinite (unitless). Source: China et al. (2017), DOI: 10.1002/2016JD025817. |
China2017_J_deposition_c_Kaolinite | -2.2209 | float | Coefficient $c$ for deposition nucleation rate $J_{het}$ of Kaolinite (unitless). Source: China et al. (2017), DOI: 10.1002/2016JD025817. |
| Name | Value | Type | Description |
|---|
J_ABIFM_m_Dust | 22.62 | float | Default empirical coefficient $m$ for the water-activity-based immersion freezing rate ($J_{het}$) parameterization for dust (unitless). |
J_ABIFM_c_Dust | -1.35 | float | Default empirical coefficient $c$ for the water-activity-based immersion freezing rate ($J_{het}$) parameterization for dust (unitless). |
J_ABIFM_m_ArizonaTestDust | 22.62 | float | Empirical coefficient $m$ for the immersion freezing rate ($J_{het}$) of Arizona Test Dust (unitless). |
J_ABIFM_c_ArizonaTestDust | -1.35 | float | Empirical coefficient $c$ for the immersion freezing rate ($J_{het}$) of Arizona Test Dust (unitless). |
J_ABIFM_m_SaharanDust | 22.62 | float | Empirical coefficient $m$ for the immersion freezing rate ($J_{het}$) of Saharan Dust (unitless). |
J_ABIFM_c_SaharanDust | -1.35 | float | Empirical coefficient $c$ for the immersion freezing rate ($J_{het}$) of Saharan Dust (unitless). |
J_ABIFM_m_AsianDust | 22.62 | float | Empirical coefficient $m$ for the immersion freezing rate ($J_{het}$) of Asian Dust (unitless). |
J_ABIFM_c_AsianDust | -1.35 | float | Empirical coefficient $c$ for the immersion freezing rate ($J_{het}$) of Asian Dust (unitless). |
J_ABIFM_m_MiddleEasternDust | 22.62 | float | Empirical coefficient $m$ for the immersion freezing rate ($J_{het}$) of Middle Eastern Dust (unitless). |
J_ABIFM_c_MiddleEasternDust | -1.35 | float | Empirical coefficient $c$ for the immersion freezing rate ($J_{het}$) of Middle Eastern Dust (unitless). |
AlpertKnopf2016_J_ABIFM_m_DesertDust | 22.62 | float | Coefficient $m$ for immersion freezing rate $J_{het}$ of Desert Dust (unitless). Source: Alpert and Knopf (2016), DOI: 10.5194/acp-16-2083-2016. |
AlpertKnopf2016_J_ABIFM_c_DesertDust | -1.35 | float | Coefficient $c$ for immersion freezing rate $J_{het}$ of Desert Dust (unitless). Source: Alpert and Knopf (2016), DOI: 10.5194/acp-16-2083-2016. |
KnopfAlpert2013_J_ABIFM_m_Kaolinite | 54.58834 | float | Coefficient $m$ for immersion freezing rate $J_{het}$ of Kaolinite (unitless). Source: Knopf and Alpert (2013), DOI: 10.1039/C3FD00035D. |
KnopfAlpert2013_J_ABIFM_c_Kaolinite | -10.54758 | float | Coefficient $c$ for immersion freezing rate $J_{het}$ of Kaolinite (unitless). Source: Knopf and Alpert (2013), DOI: 10.1039/C3FD00035D. |
KnopfAlpert2013_J_ABIFM_m_Illite | 54.48075 | float | Coefficient $m$ for immersion freezing rate $J_{het}$ of Illite (unitless). Source: Knopf and Alpert (2013), DOI: 10.1039/C3FD00035D. |
KnopfAlpert2013_J_ABIFM_c_Illite | -10.66873 | float | Coefficient $c$ for immersion freezing rate $J_{het}$ of Illite (unitless). Source: Knopf and Alpert (2013), DOI: 10.1039/C3FD00035D. |
| Name | Value | Type | Description |
|---|
p_over_sulphuric_acid_solution_T_max | 235 | float | Maximum valid temperature for the H₂SO₄ solution vapor pressure parameterization (K). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_T_min | 185 | float | Minimum valid temperature for the H₂SO₄ solution vapor pressure parameterization (K). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_w_2 | 1.4408 | float | Coefficient for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c1 | 23.306 | float | Coefficient $c_1$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c2 | 5.3465 | float | Coefficient $c_2$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c3 | 12 | float | Coefficient $c_3$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c4 | 8.19 | float | Coefficient $c_4$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c5 | -5814 | float | Coefficient $c_5$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c6 | 928.9 | float | Coefficient $c_6$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
p_over_sulphuric_acid_solution_c7 | 1876.7 | float | Coefficient $c_7$ for the H₂SO₄ solution vapor pressure parameterization (unitless). Source: Luo et al. (1995), DOI: 10.1029/94GL02988. |
| Name | Value | Type | Description |
|---|
BF1995_mass_exponent_beta | 1.9 | float | Exponent $\beta_{va}$ in the power law for mass from vapor diffusion/aggregation in the P3 scheme (unitless). Source: Brown and Francis (1995); Morrison and Milbrandt (2015). |
BF1995_mass_coeff_alpha | 7.38e-11 | float | Coefficient $\alpha_{va}$ in the power law for mass from vapor diffusion/aggregation in the P3 scheme ($g \mu m^{-\beta_{va}}$). See P3 scheme documentation to adjust units. Source: Brown and Francis (1995); Morrison and Milbrandt (2015). |
M1996_area_exponent_sigma | 1.88 | float | Exponent $\sigma$ in the power law for the projected area of various ice habits in the P3 scheme (unitless). Source: Mitchell (1996); Morrison and Milbrandt (2015). |
M1996_area_coeff_gamma | 0.2285 | float | Coefficient $\gamma$ in the power law for the projected area of various ice habits in the P3 scheme ($m^{2-\sigma}$). Source: Mitchell (1996); Morrison and Milbrandt (2015). |
Heymsfield_mu_coeff1 | 0.00191 | float | Coefficient for shape parameter $\mu$ for ice in the P3 scheme ($m^{0.8}$). Source: Morrison and Milbrandt (2015), Eq. (3). |
Heymsfield_mu_coeff2 | 0.8 | float | Coefficient for shape parameter $\mu$ for ice in the P3 scheme (unitless). Source: Morrison and Milbrandt (2015), Eq. (3). |
Heymsfield_mu_coeff3 | 2 | float | Coefficient for shape parameter $\mu$ for ice in the P3 scheme (unitless). Source: Morrison and Milbrandt (2015), Eq. (3). |
Heymsfield_mu_cutoff | 6 | float | Limiter for shape parameter $\mu$ for ice in the P3 scheme (unitless). Source: Morrison and Milbrandt (2015), Eq. (3). |
P3_constant_slope_parameterization_value | 3.0 | float | Value of $\mu$ for the constant slope parameterization in the P3 scheme (unitless). |
CL1993_local_rime_density_constant_coeff | 51 | float | Constant coefficient for local rime density in the P3 scheme (kg m⁻³). Source: Cober and List (1993), DOI: 10.1175/1520-0469(1993)050<1591:MOTHAM>2.0.CO;2. |
CL1993_local_rime_density_linear_coeff | 114 | float | Linear coefficient for local rime density in the P3 scheme (kg m⁻³ (m² s⁻¹ °C⁻¹)⁻¹). Source: Cober and List (1993), DOI: 10.1175/1520-0469(1993)050<1591:MOTHAM>2.0.CO;2. |
CL1993_local_rime_density_quadratic_coeff | -5.5 | float | Quadratic coefficient for local rime density in the P3 scheme (kg m⁻³ (m² s⁻¹ °C⁻¹)⁻²). Source: Cober and List (1993), DOI: 10.1175/1520-0469(1993)050<1591:MOTHAM>2.0.CO;2. |
P3_wet_growth_timescale | 100 | float | Timescale for densification due to wet growth in the P3 scheme (s). |
| Name | Value | Type | Description |
|---|
seasalt_aerosol_molar_mass | 0.058443 | float | Molar mass of sea salt aerosol (kg mol⁻¹). |
seasalt_aerosol_density | 2170 | float | Density of sea salt aerosol (kg m⁻³). |
seasalt_aerosol_osmotic_coefficient | 0.9 | float | Osmotic coefficient of sea salt aerosol (unitless). |
seasalt_aerosol_ion_number | 2 | float | Number of ions that sea salt dissociates into when dissolved in water (unitless). |
seasalt_aerosol_water_soluble_mass_fraction | 1 | float | Mass fraction of water-soluble material for sea salt aerosol (unitless). |
seasalt_aerosol_kappa | 1.12 | float | Hygroscopicity parameter $\kappa$ for sea salt aerosol (unitless). Source: Petters and Kreidenweis (2007), DOI: 10.5194/acp-7-1961-2007. |
MERRA2_seasalt_aerosol_bin01_radius | 7.9e-8 | float | Dry particle radius for sea salt aerosol in bin 01 of the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
MERRA2_seasalt_aerosol_bin02_radius | 3.16e-7 | float | Dry particle radius for sea salt aerosol in bin 02 of the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
MERRA2_seasalt_aerosol_bin03_radius | 1.119e-6 | float | Dry particle radius for sea salt aerosol in bin 03 of the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
MERRA2_seasalt_aerosol_bin04_radius | 2.818e-6 | float | Dry particle radius for sea salt aerosol in bin 04 of the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
MERRA2_seasalt_aerosol_bin05_radius | 7.772e-6 | float | Dry particle radius for sea salt aerosol in bin 05 of the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
sulfate_aerosol_molar_mass | 0.132 | float | Molar mass of sulfate aerosol (kg mol⁻¹). |
sulfate_aerosol_density | 1770 | float | Density of sulfate aerosol (kg m⁻³). |
sulfate_aerosol_osmotic_coefficient | 1 | float | Osmotic coefficient of sulfate aerosol (unitless). |
sulfate_aerosol_ion_number | 3 | float | Number of ions that sulfate dissociates into when dissolved in water (unitless). |
sulfate_aerosol_water_soluble_mass_fraction | 1 | float | Mass fraction of water-soluble material for sulfate aerosol (unitless). |
sulfate_aerosol_kappa | 0.53 | float | Hygroscopicity parameter $\kappa$ for sulfate aerosol (unitless). Source: Petters and Kreidenweis (2007), DOI: 10.5194/acp-7-1961-2007. |
MERRA2_sulfate_aerosol_radius | 3.5e-7 | float | Dry particle radius for sulfate aerosol in the MERRA-2 dataset (m). Source: Global Modeling and Assimilation Office (2015), DOI: 10.5067/LTVB4GPCOTK2. |
ARG2000_f_coeff_1 | 0.5 | float | Scaling coefficient for an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
ARG2000_f_coeff_2 | 2.5 | float | Scaling coefficient for an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
ARG2000_g_coeff_1 | 1.0 | float | Scaling coefficient for an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
ARG2000_g_coeff_2 | 0.25 | float | Scaling coefficient for an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
ARG2000_pow_1 | 1.5 | float | Exponent for the term $\zeta / \eta$ in an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
ARG2000_pow_2 | 0.75 | float | Exponent for the term $S_m^2 / (\zeta + 3 \eta)$ in an empirical function in the aerosol activation parameterization (unitless). Source: Abdul-Razzak and Ghan (2000), DOI: 10.1029/1999JD901161. |
| Name | Value | Type | Description |
|---|
ssa_residence | 47520.0 | float | Average residence time (s) of sea salt aerosol mass in the AeroCOM3 ensemble. Source: Gliss et al. (2021), DOI: 10.5194/acp-21-87-2021. |
ssa_size_bin_divisions | [3.0e-8, 1.0e-7, 5.0e-7, …] (6 entries) | float | Double-sided sea salt aerosol dry-radius bin edges (m) from the five-bin MERRA-2 scheme, ascending, i.e. bin1 (0.03e-6, 0.1e-6), bin2 (0.1e-6, 0.5e-6). |
ssa_r_ref | 1.0e-6 | float | Sea salt aerosol reference radius (m) used to non-dimensionalize the Gong parameterization. |
ssa_u_ref | 1.0 | float | Reference wind speed (m s⁻¹) used to non-dimensionalize the Gong parameterization. |
ssa_r80_per_dry | 2.0 | float | Ratio of the sea salt aerosol radius at 80% relative humidity to the dry radius (unitless). Source: Lewis and Schwartz (2004). |
ssa_gong_wind_exponent | 3.41 | float | Exponent on the 10 m wind speed in the Gong source function (unitless). Source: Gong (2003), DOI: 10.1029/2003GB002079. |
ssa_gong_logfit_mode1 | [0.2157, 0.05545, 17.02] | float | Lognormal mode #1 parameters: flux scale ($F$) (m⁻² s⁻¹), dry mode radius ($r$) (μm), and lognormal standard deviation ($\sigma_g$) (unitless), fit to the Gong (2003) spectrum at $u_{10}$ = ssa_u_ref. |
ssa_gong_logfit_mode2 | [60.93, 0.0914, 1.813] | float | Lognormal mode #2 parameters: flux scale ($F$) (m⁻² s⁻¹), dry mode radius ($r$) (μm), and lognormal standard deviation ($\sigma_g$) (unitless), fit to the Gong (2003) spectrum at $u_{10}$ = ssa_u_ref. |
ssa_gong_logfit_mode3 | [5.949, 0.776, 1.759] | float | Lognormal mode #3 parameters: flux scale ($F$) (m⁻² s⁻¹), dry mode radius ($r$) (μm), and lognormal standard deviation ($\sigma_g$) (unitless), fit to the Gong (2003) spectrum at $u_{10}$ = ssa_u_ref. |
ssa_gong_logfit_bin_0M_flux | [48.37, 41.92, 5.903, …] (5 entries) | float | Per-bin number flux scale (m⁻² s⁻¹) of the lognormal fit to the Gong (2003) spectrum at $u_{10}$ = ssa_u_ref. Precomputed offline in ClimaAtmos.jl/docs/sea_salt_emission_fit.jl. |
ssa_gong_logfit_bin_3M_flux | [1.589e-16, 3.575e-15, 4.557e-14, …] (5 entries) | float | Per-bin dry-mass flux scale (kg m⁻² s⁻¹) of the lognormal fit to the Gong (2003) spectrum at $u_{10}$ = ssa_u_ref. Precomputed offline in ClimaAtmos.jl/docs/sea_salt_emission_fit.jl. |
| Name | Value | Type | Description |
|---|
mam3_nucleation_p_b_n_neutral | 3.95451 | float | Empirical coefficient $p_{b,n}$ for neutral pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_p_b_i_ion_induced | 3.373738 | float | Empirical coefficient $p_{b,i}$ for ion-induced pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³ and negative ion concentration $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_u_b_n_neutral | 9.702973 | float | Empirical coefficient $u_{b,n}$ for neutral pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_u_b_i_ion_induced | -11.48166 | float | Empirical coefficient $u_{b,i}$ for ion-induced pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³ and negative ion concentration $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_v_b_n_neutral | 12.62259 | float | Empirical coefficient $v_{b,n}$ for neutral pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_v_b_i_ion_induced | 25.49469 | float | Empirical coefficient $v_{b,i}$ for ion-induced pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³ and negative ion concentration $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_w_b_n_neutral | -0.007066146 | float | Empirical coefficient $w_{b,n}$ for neutral pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_w_b_i_ion_induced | 0.1810722 | float | Empirical coefficient $w_{b,i}$ for ion-induced pure binary (H₂SO₄-H₂O) nucleation (unitless). Assumes [H₂SO₄] is in 10⁶ cm⁻³ and negative ion concentration $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_p_t_n_neutral | 2.891024 | float | Empirical coefficient $p_{t,n}$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_p_t_i_ion_induced | 3.138719 | float | Empirical coefficient $p_{t,i}$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_u_t_n_neutral | 182.4495 | float | Empirical coefficient $u_{t,n}$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_u_t_i_ion_induced | -23.8002 | float | Empirical coefficient $u_{t,i}$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_v_t_n_neutral | 1.203451 | float | Empirical coefficient $v_{t,n}$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_v_t_i_ion_induced | 37.03029 | float | Empirical coefficient $v_{t,i}$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_w_t_n_neutral | -4.188065 | float | Empirical coefficient $w_{t,n}$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_w_t_i_ion_induced | 0.227413 | float | Empirical coefficient $w_{t,i}$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_p_A_n_neutral | 8.003471 | float | Empirical coefficient $p_{A,n}$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_p_A_i_ion_induced | 3.071246 | float | Empirical coefficient $p_{A,i}$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_a_n_neutral | 1.5703478e-6 | float | Empirical coefficient $a_n$ for neutral pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄] and [NH₃] are in 10⁶ cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_a_i_ion_induced | 0.0048314 | float | Empirical coefficient $a_i$ for ion-induced pure ternary (H₂SO₄-NH₃-H₂O) nucleation (unitless). Assumes [H₂SO₄], [NH₃] are in 10⁶ cm⁻³ and $[n^-]$ is in cm⁻³. Source: Dunne et al. (2016), DOI: 10.1126/science.aaf2649. |
mam3_nucleation_a_1_neutral | 0.0400097 | float | Empirical coefficient $a_{1,n}$ for neutral pure organic nucleation (unitless). Assumes [HOM] is in 10⁷ cm⁻³ and other concentrations have units (TODO). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_a_2_neutral | 1.84826 | float | Empirical coefficient $a_{2,n}$ for neutral pure organic nucleation (unitless). Assumes [HOM] is in 10⁷ cm⁻³ and other concentrations have units (TODO). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_a_3_ion_induced | 0.00136641 | float | Empirical coefficient $a_{3,i}$ for ion-induced pure organic nucleation (unitless). Assumes [HOM] is in 10⁷ cm⁻³, $[n^-]$ in cm⁻³, and other concentrations have units (TODO). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_a_4_ion_induced | 1.56588 | float | Empirical coefficient $a_{4,i}$ for ion-induced pure organic nucleation (unitless). Assumes [HOM] is in 10⁷ cm⁻³, $[n^-]$ in cm⁻³, and other concentrations have units (TODO). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_a_5 | 0.186303 | float | Empirical coefficient $a_5$ for pure organic nucleation (unitless). Assumes [HOM] is in 10⁷ cm⁻³ and other concentrations have units (TODO). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_Y_MTO3_percent | 0.029 | float | Molar yield of highly oxygenated molecules (HOM) from monoterpene (MT) oxidation by O₃ for pure organic nucleation (%). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_Y_MTOH_percent | 0.012 | float | Molar yield of highly oxygenated molecules (HOM) from monoterpene (MT) oxidation by OH for pure organic nucleation (%). Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_k_MTO3_organic_factor | 8.05e-16 | float | Factor for temperature-dependent rate of MT oxidation by O₃ for pure organic nucleation. Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_k_MTOH_organic_factor | 1.2e-11 | float | Factor for temperature-dependent rate of MT oxidation by OH for pure organic nucleation. Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_exp_MTO3_organic_factor | -640 | float | Exponent for temperature-dependent rate of MT oxidation by O₃ for pure organic nucleation. Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_exp_MTOH_organic_factor | 440 | float | Exponent for temperature-dependent rate of MT oxidation by OH for pure organic nucleation. Source: Kirkby et al. (2016), DOI: 10.1038/nature17953. |
mam3_nucleation_k_H2SO4_mixed_organic_sulfuric_acid_factor | 3.27e-21 | float | Temperature-dependent factor for mixed organic-sulfuric acid nucleation. Assumes [H₂SO₄] is in 10⁶ cm⁻³ and [BioOxOrg] is in cm⁻³. Source: Riccobono et al. (2014), DOI: 10.1126/science.1243527. |
| Name | Value | Type | Description |
|---|
idealized_ocean_albedo | 0.38 | float | Ocean surface albedo for idealized simulations (unitless). Source: O'Gorman and Schneider (2008). |
water_refractive_index | 1.34 | float | Relative refractive index of water and air for broadband ocean surface albedo calculation (unitless). Source: Jin et al. (2011). |
optics_lookup_temperature_min | 160 | float | Minimum temperature in the lookup table for optical properties in RRTMGP (K). |
optics_lookup_temperature_max | 355 | float | Maximum temperature in the lookup table for optical properties in RRTMGP (K). |
CO2_fixed_value | 0.000397547 | float | Global mean mole fraction to fix carbon dioxide (CO₂) when using a fixed CO₂ model. Taken from the first value of 'carbon_dioxide_GM' in RRTMGP (mol mol⁻¹). |
N2O_fixed_value | 3.2699e-7 | float | Global mean mole fraction of nitrous oxide (N₂O). Taken from the first value of 'nitrous_oxide_GM' in RRTMGP (mol mol⁻¹). |
CO_fixed_value | 1.2e-7 | float | Global mean mole fraction of carbon monoxide (CO). Taken from the first value of 'carbon_monoxide_GM' in RRTMGP (mol mol⁻¹). |
CH4_fixed_value | 1.8315e-6 | float | Global mean mole fraction of methane (CH₄). Taken from the first value of 'methane_GM' in RRTMGP (mol mol⁻¹). |
O2_fixed_value | 0.209 | float | Global mean mole fraction of oxygen (O₂). Taken from the first value of 'oxygen_GM' in RRTMGP (mol mol⁻¹). |
N2_fixed_value | 0.781 | float | Global mean mole fraction of nitrogen (N₂). Taken from the first value of 'nitrogen_GM' in RRTMGP (mol mol⁻¹). |
CCL4_fixed_value | 8.307e-11 | float | Global mean mole fraction of carbon tetrachloride (CCl₄). Taken from the first value of 'carbon_tetrachloride_GM' in RRTMGP (mol mol⁻¹). |
CFC11_fixed_value | 2.3308e-10 | float | Global mean mole fraction of chlorofluorocarbon CFC11. Taken from the first value of 'cfc11_GM' in RRTMGP (mol mol⁻¹). |
CFC12_fixed_value | 5.2058e-10 | float | Global mean mole fraction of chlorofluorocarbon CFC12. Taken from the first value of 'cfc12_GM' in RRTMGP (mol mol⁻¹). |
CFC22_fixed_value | 2.2954e-10 | float | Global mean mole fraction of hydrochlorofluorocarbon CFC22. Taken from the first value of 'hcfc22_GM' in RRTMGP (mol mol⁻¹). |
HFC143A_fixed_value | 1.5253e-11 | float | Global mean mole fraction of hydrofluorocarbon HFC143A. Taken from the first value of 'hfc143a_GM' in RRTMGP (mol mol⁻¹). |
HFC125_fixed_value | 1.5355e-11 | float | Global mean mole fraction of hydrofluorocarbon HFC125. Taken from the first value of 'hfc125_GM' in RRTMGP (mol mol⁻¹). |
HFC23_fixed_value | 2.689e-11 | float | Global mean mole fraction of hydrofluorocarbon HFC23. Taken from the first value of 'hfc23_GM' in RRTMGP (mol mol⁻¹). |
HFC32_fixed_value | 8.337e-12 | float | Global mean mole fraction of hydrofluorocarbon HFC32. Taken from the first value of 'hfc32_GM' in RRTMGP (mol mol⁻¹). |
HFC134A_fixed_value | 8.0516e-11 | float | Global mean mole fraction of hydrofluorocarbon HFC134A. Taken from the first value of 'hfc134a_GM' in RRTMGP (mol mol⁻¹). |
CF4_fixed_value | 8.1092e-11 | float | Global mean mole fraction of carbon tetrafluoride (CF₄). Taken from the first value of 'cf4_GM' in RRTMGP (mol mol⁻¹). |
NO2_fixed_value | 0 | float | Global mean mole fraction of nitrogen dioxide (NO₂) (mol mol⁻¹). |
| Name | Value | Type | Description |
|---|
ogw_mountain_height_width_exponent | 0.4 | float | Mountain height-width exponent $\gamma$ in $L \propto h^\gamma$ (unitless); the paper suggests $\gamma \approx 0.4$. Source: Garner (2005), Eq. (14), DOI: 10.1175/JAS3496.1. |
ogw_number_density_exponent | 0.0 | float | Number density exponent $\epsilon$, where the number density of orography in a grid cell is $n(h) \propto h^{-\epsilon}$ (unitless). Source: Garner (2005), DOI: 10.1175/JAS3496.1. |
ogw_mountain_shape_parameter | 0.5 | float | Mountain shape parameter $\beta$ (unitless) in $L(z) = L_b (1 - z/h)^\beta$: $\beta = 1$ for triangular mountains, $\beta < 1$ for blunt mountains, and $\beta > 1$ for pointy mountains. Source: Garner (2005), Eq. (12), DOI: 10.1175/JAS3496.1. |
ogw_critical_height_threshold | 0.1 | float | Fractional height threshold $h_\text{frac}$ in $h_\text{crit} = h_\text{frac} (V / N)$, demarcating the split between propagating and non-propagating orographic gravity waves (unitless). Source: Garner (2005), DOI: 10.1175/JAS3496.1. |
ogw_density_scale_factor | 1.2 | float | Density scale factor $\rho_\text{scale}$. Source: Garner (2005), DOI: 10.1175/JAS3496.1. |
ogw_reference_mountain_width | 80000.0 | float | Reference mountain width $L_0$ (m). Source: Garner (2005), DOI: 10.1175/JAS3496.1. |
ogw_linear_drag_coefficient | 0.9 | float | Linear drag coefficient $a_0$ (unitless). Source: Garner (2005), Eq. (13), DOI: 10.1175/JAS3496.1. |
ogw_nonlinear_drag_coefficient | 3.0 | float | Nonlinear drag coefficient $a_1$ (unitless). Source: Garner (2005), Eq. (13), DOI: 10.1175/JAS3496.1. |
ogw_critical_froude_number | 0.7 | float | Critical Froude number $Fr_\text{crit}$, computed from the critical height threshold (unitless). Source: Garner (2005), DOI: 10.1175/JAS3496.1. |
ogw_smoothing_scale_fraction | 0.15 | float | Orographic gravity wave (raw_topo) preprocessing smoothing scale as a fraction of grid spacing: L = α·Δx. Sets the neighborhood over which subgrid mountain statistics (hmax and velocity potential χ / orographic tensor) are computed from raw topography, following Garner (2005) / GFDL topo_drag. α≈1 places L near the grid scale. |
| Name | Value | Type | Description |
|---|
nogw_source_pressure | 31500.0 | float | Source level pressure (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_damp_pressure | 85.0 | float | Damping level pressure (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_source_height | 15000.0 | float | Source level height (m). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bw | 0.4 | float | Westward wave spectral amplitude (m² s⁻²). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bn | 0.0 | float | Northward wave spectral amplitude (m² s⁻²). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_dc | 0.8 | float | Phase speed resolution (m s⁻¹). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_cmax | 100.0 | float | Maximum phase speed (m s⁻¹). The phase-speed grid is $c[n] = (n-1)\,\Delta c - c_\text{max}$, so an exact $c = 0$ bin exists only when nogw_cmax divided by nogw_dc is an integer; this is required for the Beres steady ($\nu = 0$) convective source, which deposits there and silently no-ops otherwise. The default, 100.0 / 0.8 = 125, gives a $c = 0$ bin. Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_c0 | 0.0 | float | Reference phase speed (m s⁻¹). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_nk | 1.0 | float | Number of wave bands (unitless). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_cw | 35.0 | float | Westward phase speed half-width (m s⁻¹). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_cw_tropics | 35.0 | float | Tropical westward phase speed half-width (m s⁻¹). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_cn | 2.0 | float | Northward phase speed half-width (m s⁻¹). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bt_0 | 0.0043 | float | Base total source momentum flux (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bt_n | 0.0 | float | Northern hemisphere total momentum flux amplitude (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bt_s | 0.0 | float | Southern hemisphere total momentum flux amplitude (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_Bt_eq | 0.0043 | float | Equatorial total momentum flux amplitude (Pa). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_phi0_n | 15.0 | float | Northern hemisphere latitude center (degrees). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_phi0_s | -15.0 | float | Southern hemisphere latitude center (degrees). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_dphi_n | 10.0 | float | Northern hemisphere latitude width (degrees). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_dphi_s | -10.0 | float | Southern hemisphere latitude width (degrees). Source: Alexander and Dunkerton (1999), DOI: 10.1175/1520-0469(1999)056<4167:ASPOMF>2.0.CO;2. |
nogw_beres_Q0_threshold | 1.0e-5 | float | Minimum convective heating rate to activate the Beres et al. (2004) convective gravity-wave source (K s⁻¹, ~1 K day⁻¹ = 1e-5). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOSTG>2.0.CO;2. |
nogw_beres_scale_factor | 2.0e-6 | float | Amplitude scaling for the Beres convective momentum flux (unitless); folds the rho_0/(L*tau) prefactor, the |Q_t|^2 weight, and empirical tuning into one parameter. Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_sigma_x | 4000.0 | float | Convective cell horizontal half-width (m) in the Beres source spectrum (Eq. 7). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_nu_min | 0.0008727 | float | Minimum angular frequency for the Beres frequency integration (rad s⁻¹, period ~120 min). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_nu_max | 0.01047 | float | Maximum angular frequency for the Beres frequency integration (rad s⁻¹, period ~10 min). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_n_nu | 9 | integer | Number of quadrature points for the Beres frequency integration (unitless; must be 4k+1: 5, 9, 13, ... for composite Boole's rule). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_h_heat_min | 1000.0 | float | Minimum heating depth (m) to activate the Beres source; filters out shallow convection. Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_n_h_avg | 1 | integer | Number of heating depths h over which to average the Beres spectrum (unitless; 1 = no averaging, >=3 smooths the resonance peak, see Fig. 4 of the source). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_delta_h_frac | 0.1 | float | Fractional half-range for Beres $h$ averaging, $h \pm$ nogw_beres_delta_h_frac $\cdot h$ (unitless); only used when nogw_beres_n_h_avg > 1. Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_z_bot_Q_threshold | 1.157e-5 | float | Minimum Q_conv to count as the bottom of the Beres convective heating envelope (K s⁻¹, ~1 K day⁻¹ = 1.157e-5). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_z_bot_floor | 2000.0 | float | Minimum allowed Beres convective envelope bottom (m); excludes the PBL-turbulence signal in Q_conv. Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_steady_dc_frac | 1.0 | float | Steady Beres DC heating weight (unitless) in $Q_t(0)^2 =$ nogw_beres_steady_dc_frac $\cdot \nu_\text{min}$; scales the steady-vs-transient amplitude. Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
nogw_beres_L_system | 1.0e6 | float | Largest convective-system scale (m) setting k_min = 2*pi/L in the even-folded horizontal constant H of the steady Beres source (steady/transient ratio depends on it only logarithmically). Source: Beres et al. (2004), DOI: 10.1175/1520-0469(2004)061<0324:AMOICG>2.0.CO;2. |
| Name | Value | Type | Description |
|---|
CO2_compensation_point_25c | 4.275e-5 | float | CO₂ compensation point ($\Gamma^*$) at 25°C (mol mol⁻¹). Source: Bernacchi et al. (2001). |
CO2_michaelis_menten | 0.0004049 | float | Michaelis-Menten parameter for CO₂ at 25°C (mol mol⁻¹). Source: Bernacchi et al. (2001). |
O2_michaelis_menten | 0.2784 | float | Michaelis-Menten parameter for O₂ at 25°C (mol mol⁻¹). Source: Bernacchi et al. (2001). |
CO2_activation_energy | 79430.0 | float | Energy of activation for CO₂ (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
O2_activation_energy | 36380.0 | float | Energy of activation for oxygen (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
Vcmax_activation_energy | 65330.0 | float | Energy of activation for Vcmax (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
Γstar_activation_energy | 37830.0 | float | Energy of activation for $\Gamma^*$ (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
Jmax_activation_energy | 43540.0 | float | Energy of activation for Jmax (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
Rd_activation_energy | 46390.0 | float | Energy of activation for dark respiration, Rd (J mol⁻¹). Source: Bonan (2019), Table 11.2; Bernacchi et al. (2001, 2003). |
kelvin_25C | 298.15 | float | Reference temperature equal to 25°C (K). |
intercellular_O2_concentration | 0.209 | float | Intercellular O₂ concentration, assumed constant (mol mol⁻¹). |
photosystem_II_quantum_yield | 0.7 | float | Quantum yield of photosystem II (unitless). Source: Bonan (2019); Bernacchi et al. (2003). |
Farquhar_curvature_parameter | 0.9 | float | Curvature parameter for calculating $J$, a fitting constant (unitless). Source: von Caemmerer (2000, 2013); Bernacchi et al. (2003, 2013); von Caemmerer et al. (2009). |
dark_respiration_factor | 0.015 | float | Constant factor appearing in the dark respiration term (unitless). Source: Bonan (2019). |
low_water_pressure_sensitivity | 5.0e-6 | float | Sensitivity of stomatal conductance to low water pressure (Pa⁻¹). |
moisture_stress_ref_water_pressure | -2.0e6 | float | Reference water pressure for the moisture stress factor (Pa). Source: Tuzet et al. (2003). |
electron_transport_maintenance | 0.05336251 | float | Constant describing the cost of maintaining electron transport (unitless). |
| Name | Value | Type | Description |
|---|
thermal_conductivity_of_quartz | 8.0 | float | Thermal conductivity of quartz (W m⁻¹ K⁻¹). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
thermal_conductivity_of_soil_minerals | 2.5 | float | Thermal conductivity of soil minerals, excluding quartz (W m⁻¹ K⁻¹). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
thermal_conductivity_of_organic_matter | 0.25 | float | Thermal conductivity of organic matter (W m⁻¹ K⁻¹). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
thermal_conductivity_of_liquid_water | 0.57 | float | Thermal conductivity of liquid water at 10°C (W m⁻¹ K⁻¹). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
thermal_conductivity_of_water_ice | 2.21 | float | Thermal conductivity of water ice at its freezing temperature (W m⁻¹ K⁻¹). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
kersten_number_alpha | 0.24 | float | Empirical constant $\alpha$ used in computing the Kersten number (unitless). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
kersten_number_beta | 18.3 | float | Empirical constant $\beta$ used in computing the Kersten number (unitless). Source: Balland and Arp (2005), DOI: 10.1139/s05-007. |
ice_impedance_omega | 7.0 | float | Impedance parameter $\Omega$ used to adjust soil hydraulic conductivity for ice presence (unitless). Source: Lundin (1990), DOI: 10.1016/0022-1694(90)90264-X. |
temperature_factor_soil_hydraulic_conductivity | 0.0264 | float | An empirical parameter for adjusting soil hydraulic conductivity based on temperature (K⁻¹). |
temperature_reference_soil_hydraulic_conductivity | 288 | float | The reference temperature for adjusting soil hydraulic conductivity (K). |
maximum_dry_soil_layer_depth | 0.015 | float | Maximum depth of the dry soil layer that can develop under evaporation (m). Source: Shokri and Or (2011), DOI: 10.1029/2010WR010284. |
emissivity_bare_soil | 0.96 | float | Emissivity of bare soil (unitless). Source: CLM5 Technical Note (2020). |