Variables | |
const double | undefined = -999. |
This is the snowpack undefined value. More... | |
const int | iundefined = -999 |
This is the snowpack undefined value. More... | |
const size_t | stundefined = static_cast<size_t>(-999) |
const double | min_percent_values = 0.9 |
const double | pi = 3.14159265358979323846 |
const double | g = 9.80665 |
const double | stefan_boltzmann = 5.67051e-8 |
const double | solcon = 1366.1 |
Total Solar Irradiance (W m-2) (Froehlich, 2006) More... | |
const double | gas_constant = 461.9 |
(J kg-1 K-1) More... | |
const double | gas_constant_air = 287.0 |
for air (J kg-1 K-1) More... | |
const double | gas_constant_mol = 8.31 |
(J mol-1 K-1) More... | |
const double | karman = 0.4 |
Karman constant. More... | |
Albedo (1) | |
const double | min_albedo = 0.3 |
const double | max_albedo = 0.9 |
const double | glacier_albedo = 0.3 |
Emissivity (1) | |
const double | emissivity_snow = 0.98 |
const double | emissivity_soil = 0.95 |
Density (kg m-3) | |
const double | density_air = 1.1 |
Approximation: use ideal gas law. More... | |
const double | density_ice = 917.0 |
At T = 0 degC. More... | |
const double | density_water = 1000.0 |
At T = 0 degC. More... | |
const double | density_vapor = 1.0 |
Approximation: use ideal gas law. More... | |
Specific heat (J kg-1 K-1) | |
const double | specific_heat_ice = 2100.0 |
at T = 0 degC More... | |
const double | specific_heat_water = 4190.0 |
at T = 0 degC More... | |
const double | specific_heat_air = 1004.67 |
see Stull "Meteorology for scientists and engineers" p44 More... | |
Thermal conductivity of snow components ice, water and air (W m-1 K-1) | |
const double | conductivity_ice = 2.2 |
(W m-1 K-1) More... | |
const double | conductivity_water = 0.598 |
(W m-1 K-1) More... | |
const double | conductivity_air = 0.026 |
(W m-1 K-1) More... | |
Vapor Diffusion in Air and Snow (m2 s-1) | |
const double | diffusion_coefficient_in_air = 22.0e-6 |
This value was taken from: Colbeck, S.C., 1993. The vapor diffusion coefficient for snow, Water Resources Research, 29(1) More... | |
const double | diffusion_coefficient_in_snow = 85.0e-6 |
It is larger (see Colbeck) according to work prior to 2008! More... | |
Phase change constants | |
const double | meltfreeze_tk = 273.15 |
(K) More... | |
const double | triple_point_t = 273.16 |
(K) More... | |
const double | triple_point_p = 611.73 |
(Pa) More... | |
const double | lh_sublimation = 2.838e6 |
(J kg-1) (solid to vapor) More... | |
const double | lh_vaporization = 2.504e6 |
(J kg-1) (liquid to vapor) More... | |
const double | lh_fusion = 3.34e5 |
(J kg-1) (solid to liquid) More... | |
Numerical Constants | |
const double | min_slope_angle = 3. |
Smallest angle a flat field may show (deg) More... | |
const double | eps = 1.e-6 |
Small numbers for comparisons and to avoid divisions by zero. More... | |
const double | eps2 = eps*eps |
const double | big = 1.0e200 |
used for Dirichlet boundary conditions More... | |
const double Constants::big = 1.0e200 |
used for Dirichlet boundary conditions
const double Constants::conductivity_air = 0.026 |
(W m-1 K-1)
const double Constants::conductivity_ice = 2.2 |
(W m-1 K-1)
const double Constants::conductivity_water = 0.598 |
(W m-1 K-1)
const double Constants::density_air = 1.1 |
Approximation: use ideal gas law.
const double Constants::density_ice = 917.0 |
At T = 0 degC.
const double Constants::density_vapor = 1.0 |
Approximation: use ideal gas law.
const double Constants::density_water = 1000.0 |
At T = 0 degC.
const double Constants::diffusion_coefficient_in_air = 22.0e-6 |
This value was taken from: Colbeck, S.C., 1993. The vapor diffusion coefficient for snow, Water Resources Research, 29(1)
const double Constants::diffusion_coefficient_in_snow = 85.0e-6 |
It is larger (see Colbeck) according to work prior to 2008!
const double Constants::emissivity_snow = 0.98 |
const double Constants::emissivity_soil = 0.95 |
const double Constants::eps = 1.e-6 |
Small numbers for comparisons and to avoid divisions by zero.
const double Constants::g = 9.80665 |
const double Constants::gas_constant = 461.9 |
(J kg-1 K-1)
const double Constants::gas_constant_air = 287.0 |
for air (J kg-1 K-1)
const double Constants::gas_constant_mol = 8.31 |
(J mol-1 K-1)
const double Constants::glacier_albedo = 0.3 |
const int Constants::iundefined = -999 |
This is the snowpack undefined value.
const double Constants::karman = 0.4 |
Karman constant.
const double Constants::lh_fusion = 3.34e5 |
(J kg-1) (solid to liquid)
const double Constants::lh_sublimation = 2.838e6 |
(J kg-1) (solid to vapor)
const double Constants::lh_vaporization = 2.504e6 |
(J kg-1) (liquid to vapor)
const double Constants::max_albedo = 0.9 |
const double Constants::meltfreeze_tk = 273.15 |
(K)
const double Constants::min_albedo = 0.3 |
const double Constants::min_percent_values = 0.9 |
const double Constants::min_slope_angle = 3. |
Smallest angle a flat field may show (deg)
const double Constants::pi = 3.14159265358979323846 |
const double Constants::solcon = 1366.1 |
Total Solar Irradiance (W m-2) (Froehlich, 2006)
const double Constants::specific_heat_air = 1004.67 |
see Stull "Meteorology for scientists and engineers" p44
const double Constants::specific_heat_ice = 2100.0 |
at T = 0 degC
const double Constants::specific_heat_water = 4190.0 |
at T = 0 degC
const double Constants::stefan_boltzmann = 5.67051e-8 |
const size_t Constants::stundefined = static_cast<size_t>(-999) |
const double Constants::triple_point_p = 611.73 |
(Pa)
const double Constants::triple_point_t = 273.16 |
(K)
const double Constants::undefined = -999. |
This is the snowpack undefined value.