| MadSci Network: Earth Sciences |
The proper way to deal with this question involves differential equations with Newton's law of heating/cooling. However, it is impossible to answer this question based on the information provided. To properly answer your question, we would have to develop a sophisticated model that incorporates the size and shape of the lake, inventory all of the sources and sinks of heat, measure the vertical temperature profile, and estimate convective processes in the lake, just to name a few. We would also have to know a lot more about the composition of the lake water including its turbidity and salinity (colligative properties affect freezing temperature), effective heat conductivity, etc. Measurements like the 10" of ice is not very useful unless we know how deep the lake is at the place where the 10" of ice was measured. You'll find that the thickness of the ice will vary, increasing near the shallower and stagnant areas of the lake. Also, what is the long term temperature history of the area? Large bodies of water can store lots of heat. While freezing the top layer may just take a cold snap, significantly altering its average and deep water temperature takes a longer period of cooling. To put your question in a more mathematical form, I think you're asking what is dz/dt of ice, where z(0) is the surface and decreases with depth. The first order equation, neglecting all of the complexity I previously mentioned, relates dz/dt with the rate of cooling/heating (dH/dt). You would have to make plenty of assumptions and in the end any scientist would probably end up pretty embarrassed of how inadequate their model is stacked up against reality. A more accurate engineering approach involves using statistics to correlate the thickness of the ice with the temperature of the ground and air, but even here, your answer would vary depending on depth of the lake at which the measurement was made and how deep into winter the cold snap came. Sorry, but there is no simple answer to this question.
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