Heating the upper layer of water during thermal conductivity measurements is primarily to prevent convection, which can interfere with accurate conduction measurements. Convection occurs when warm water rises and cold water sinks, driven by gravity, and heating from the top eliminates this effect. The goal is to isolate heat conduction as the sole method of heat transfer, as conduction is not influenced by gravity. While it may seem that keeping the upper layer hot aids conduction, the key point is that conduction operates independently of gravitational forces. Therefore, maintaining a hot upper layer is essential for accurate measurement of thermal conductivity without the interference of convection.