dallaston2015_melt Interface

The inverse stefan number, $$\frac{c(T_a - T_m)}{L}$$

The factor to convert between the scale for melt used by Dallaston et al. (2015) and that used in ISOFT, $$\frac{m_0x_0}{D_0U_0},$$ where $m_0$ is the melt scale used by Dalalston et al.

The factor which, when used to divide the melt_conversion term, produces a conversion factor for the melt-terms in the salinity equation of Dallaston et al. (2015). It has the form $$\frac{Q_{g0}}{D_0U_0},$$ where $Q_{g0}$ is the subglacial discharge across the grounding line.