Thermodynamic + turbulence constants. All SI.
DENSITY TRAP: rho_w multiplies the OCEAN-side turbulent fluxes
in (E2)/(E3); rho_i and rho_fw are used ONLY to convert the
canonical mass flux into a thickness rate for REPORTING. They
are three different numbers in three different papers and must
never be interchanged.
Defaults are the ISOMIP+ protocol set (Asay-Davis et al. (2016) Table 4 p. 2483) plus the turbulence constants that protocol does not specify, taken from Holland & Jenkins (1999) Table 1 p. 1790 and Yung et al. (2025) Table A1 p. 5849.
| Type | Visibility | Attributes | Name | Initial | |||
|---|---|---|---|---|---|---|---|
| real(kind=wp), | public | :: | L_f | = | 3.34e5_wp |
Latent heat of fusion (J/kg) — Holland & Jenkins (1999) Table 1 p. 1790; Asay-Davis et al. (2016) Table 4 p. 2483; Yung et al. (2025) Table 1 p. 5832. (Burchard et al. (2022) Table 1 p. 8 uses 3.335e5.) |
|
| real(kind=wp), | public | :: | Pr | = | 13.8_wp |
Molecular Prandtl number — Holland & Jenkins (1999) Table 1 p. 1790, confirmed by McPhee, Maykut & Morison (1987) p. 7029. |
|
| real(kind=wp), | public | :: | R_c | = | 0.20_wp |
Critical flux Richardson number — Holland & Jenkins (1999) Table 1 p. 1790. |
|
| real(kind=wp), | public | :: | Sc | = | 2432.0_wp |
Molecular Schmidt number — same two sources. |
|
| real(kind=wp), | public | :: | alpha_T | = | 3.733e-5_wp |
FRACTIONAL thermal expansion coefficient (1/degC) of the
ISOMIP+ linear EOS — Asay-Davis et al. (2016) Table 4 p. 2483.
Feeds the interfacial buoyancy flux only. NOTE
|
|
| real(kind=wp), | public | :: | beta_S | = | 7.843e-4_wp |
FRACTIONAL haline contraction coefficient (1/(g/kg)) of the ISOMIP+ linear EOS — Asay-Davis et al. (2016) Table 4 p. 2483. |
|
| real(kind=wp), | public | :: | c_i | = | 2009.0_wp |
Specific heat capacity of ice (J/kg/K) — Holland & Jenkins
(1999) Table 1 p. 1790. Read only by |
|
| real(kind=wp), | public | :: | c_w | = | 3974.0_wp |
Specific heat capacity of seawater (J/kg/K) — unanimous across Holland & Jenkins (1999), Jenkins et al. (2010), Asay-Davis et al. (2016) and Yung et al. (2025). |
|
| real(kind=wp), | public | :: | g | = | 9.81_wp |
Gravitational acceleration (m/s^2), as used by the buoyancy flux — Asay-Davis et al. (2016) Table 4 p. 2483. |
|
| real(kind=wp), | public | :: | kappa_vk | = | 0.40_wp |
Von Karman constant — Holland & Jenkins (1999) Table 1
p. 1790. Also the |
|
| real(kind=wp), | public | :: | nu | = | 1.95e-6_wp |
Kinematic viscosity of seawater (m^2/s) — Holland & Jenkins (1999) Table 1 p. 1790. |
|
| real(kind=wp), | public | :: | rho_fw | = | 1000.0_wp |
Freshwater density (kg/m^3), REPORTING ONLY — the density
ISOMIP+ reports its |
|
| real(kind=wp), | public | :: | rho_i | = | 918.0_wp |
Ice density (kg/m^3), REPORTING ONLY — Asay-Davis et al. (2016) p. 2479 and Yung et al. (2025). |
|
| real(kind=wp), | public | :: | rho_w | = | 1028.0_wp |
Seawater density multiplying the turbulent fluxes (kg/m^3) — Asay-Davis et al. (2016) p. 2479. The papers span 1025 (H&J99) to 1030 (Jenkins et al. 2010), a 0.5% spread that lands directly on the melt rate. |
|
| real(kind=wp), | public | :: | xi_N | = | 0.052_wp |
McPhee stability constant |
type :: ocean_cavity_const_t !! Thermodynamic + turbulence constants. All SI. !! !! DENSITY TRAP: `rho_w` multiplies the OCEAN-side turbulent fluxes !! in (E2)/(E3); `rho_i` and `rho_fw` are used ONLY to convert the !! canonical mass flux into a thickness rate for REPORTING. They !! are three different numbers in three different papers and must !! never be interchanged. !! !! Defaults are the ISOMIP+ protocol set (Asay-Davis et al. (2016) !! Table 4 p. 2483) plus the turbulence constants that protocol does !! not specify, taken from Holland & Jenkins (1999) Table 1 p. 1790 !! and Yung et al. (2025) Table A1 p. 5849. real(wp) :: L_f = 3.34e5_wp !! Latent heat of fusion (J/kg) — Holland & Jenkins (1999) !! Table 1 p. 1790; Asay-Davis et al. (2016) Table 4 p. 2483; !! Yung et al. (2025) Table 1 p. 5832. (Burchard et al. (2022) !! Table 1 p. 8 uses 3.335e5.) real(wp) :: c_w = 3974.0_wp !! Specific heat capacity of seawater (J/kg/K) — unanimous across !! Holland & Jenkins (1999), Jenkins et al. (2010), Asay-Davis et !! al. (2016) and Yung et al. (2025). real(wp) :: c_i = 2009.0_wp !! Specific heat capacity of ice (J/kg/K) — Holland & Jenkins !! (1999) Table 1 p. 1790. Read only by `CAVITY_ICE_ADV_DIFF`. real(wp) :: rho_w = 1028.0_wp !! Seawater density multiplying the turbulent fluxes (kg/m^3) — !! Asay-Davis et al. (2016) p. 2479. The papers span 1025 (H&J99) !! to 1030 (Jenkins et al. 2010), a 0.5% spread that lands !! directly on the melt rate. real(wp) :: rho_i = 918.0_wp !! Ice density (kg/m^3), REPORTING ONLY — Asay-Davis et al. !! (2016) p. 2479 and Yung et al. (2025). real(wp) :: rho_fw = 1000.0_wp !! Freshwater density (kg/m^3), REPORTING ONLY — the density !! ISOMIP+ reports its `m_w` melt rate with (Asay-Davis et al. !! (2016) eq. (24) p. 2485). real(wp) :: alpha_T = 3.733e-5_wp !! FRACTIONAL thermal expansion coefficient (1/degC) of the !! ISOMIP+ linear EOS — Asay-Davis et al. (2016) Table 4 p. 2483. !! Feeds the interfacial buoyancy flux only. NOTE !! `eos_t%alpha_T` in this repository is DIMENSIONAL (kg/m^3 per !! degC) = `rho0` times this; convert at the coupling seam. !! OPEN QUESTION, recorded not resolved: near -2 degC the true !! thermal expansion under a nonlinear EOS is near zero or !! NEGATIVE, which flips the sign of the (small) temperature term !! in the buoyancy flux and therefore of the stratification !! feedback near neutrality. No paper in the set addresses it. real(wp) :: beta_S = 7.843e-4_wp !! FRACTIONAL haline contraction coefficient (1/(g/kg)) of the !! ISOMIP+ linear EOS — Asay-Davis et al. (2016) Table 4 p. 2483. real(wp) :: g = 9.81_wp !! Gravitational acceleration (m/s^2), as used by the buoyancy !! flux — Asay-Davis et al. (2016) Table 4 p. 2483. real(wp) :: nu = 1.95e-6_wp !! Kinematic viscosity of seawater (m^2/s) — Holland & Jenkins !! (1999) Table 1 p. 1790. real(wp) :: Pr = 13.8_wp !! Molecular Prandtl number — Holland & Jenkins (1999) Table 1 !! p. 1790, confirmed by McPhee, Maykut & Morison (1987) p. 7029. real(wp) :: Sc = 2432.0_wp !! Molecular Schmidt number — same two sources. real(wp) :: kappa_vk = 0.40_wp !! Von Karman constant — Holland & Jenkins (1999) Table 1 !! p. 1790. Also the `kappa` of the Obukhov scale. real(wp) :: xi_N = 0.052_wp !! McPhee stability constant `xi_N` — Holland & Jenkins (1999) !! Table 1 p. 1790; McPhee, Maykut & Morison (1987) p. 7029; Yung !! et al. (2025) Table A1 p. 5849. (NOT 0.13: no paper in the !! set contains a `zeta_N` or that value.) real(wp) :: R_c = 0.20_wp !! Critical flux Richardson number — Holland & Jenkins (1999) !! Table 1 p. 1790. end type ocean_cavity_const_t