PISM, A Parallel Ice Sheet Model 2.2.2-d6b3a29ca committed by Constantine Khrulev on 2025-03-28
|
◆ L()Latent heat of fusion of water as a function of pressure melting temperature. Following a re-interpretation of [AschwandenBuelerKhroulevBlatter], we require that \Diff{H}{p} = 0 : \Diff{H}{p} = \diff{H_w}{p} + \diff{H_w}{p}\Diff{T}{p} We assume that water is incompressible, so \Diff{T}{p} = 0 and the second term vanishes. As for the first term, equation (5) of [AschwandenBuelerKhroulevBlatter] defines H_w as follows: H_w = \int_{T_0}^{T_m(p)} C_i(t) dt + L + \int_{T_m(p)}^T C_w(t)dt Using the fundamental theorem of Calculus, we get \diff{H_w}{p} = (C_i(T_m(p)) - C_w(T_m(p))) \diff{T_m(p)}{p} + \diff{L}{p} Assuming that C_i(T) = c_i and C_w(T) = c_w (i.e. specific heat capacities of ice and water do not depend on temperature) and using the Clausius-Clapeyron relation T_m(p) = T_m(p_{\text{air}}) - \beta p, we get \begin{align} \Diff{H}{p} &= (c_i - c_w)\diff{T_m(p)}{p} + \diff{L}{p}\\ &= \beta(c_w - c_i) + \diff{L}{p}\\ \end{align} Requiring \Diff{H}{p} = 0 implies \diff{L}{p} = -\beta(c_w - c_i), and so \begin{align} L(p) &= -\beta p (c_w - c_i) + C\\ &= (T_m(p) - T_m(p_{\text{air}})) (c_w - c_i) + C. \end{align} Letting p = p_{\text{air}} we find C = L(p_\text{air}) = L_0 , so L(p) = (T_m(p) - T_m(p_{\text{air}})) (c_w - c_i) + L_0, where L_0 is the latent heat of fusion of water at atmospheric pressure. Therefore a consistent interpretation of [AschwandenBuelerKhroulevBlatter] requires the temperature-dependent approximation of the latent heat of fusion of water given above. Note that this form of L(p) also follows from Kirchhoff's law of thermochemistry. Definition at line 364 of file EnthalpyConverter.cc. |