If the level of water in a calorimeter has become higher, it means that a part of water has been frozen (the volume of water increases during freezing). On the other hand, we can state that some amount of water has not been frozen since otherwise its volume would have increased by a factor of ρw/ρice ≈ 1.1, and the level of water in the calorimeter would have increased by (h/3) (1.1 - 1) ≈ 2.5 cm, while by hypothesis Δh = 0.5 cm. Thus, the temperature established in the calorimeter is 0 °C.
Using this condition, we can write

where Δm is the mass of frozen water, and Tice is the initial temperature of ice. As was mentioned above, the volume of water increases as a result of freezing by a factor of ρw/ρice, and hence

where S is the cross-sectional area of the calorimeter. Substituting Δm from Eq. (2) into Eq. (1) and using the relations mw (h/3)ρwS and mice = (h/3) ρiceS, we obtain
