The heat that the lake losses is used to melt the ice (since it is already at melting temperature), and heat the water from ice from zero degrees to equilibrium temperature.
Hence, the balance equation is , where
is the initial temperature of the lake, is the equilibrium temperature (of both lake water and ice water after melting), is the melting point of the ice, is the latent heat of melting of ice, is the specific heat capacity of ice.
From the last equation, the mass of the water is .
The heat lost by the lake is the quantity either in the left, or the right hand side of the balance equation, and is equal to .
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