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The discussion centers on the optimal conditions for packing snow to create a snowman, specifically emphasizing that snow packs best when temperatures are just above freezing. The unique properties of water, including its expansion upon freezing, play a crucial role in this process. Participants share personal experiences, noting that wet snow, which typically occurs near the melting point, is essential for effective packing. The conversation also highlights misconceptions about snow packing, with some contributors arguing that the wetness of the snow is more significant than temperature alone.
PREREQUISITESThis discussion is beneficial for winter sports enthusiasts, meteorologists, educators teaching about phase changes, and anyone interested in the science behind snow and its properties.
I can see that. It seems you used up all the available snow.Charles Link said:Packing conditions were good, but I had very little snow to work with.
I'm impressed that we had to come this far into the thread for someone to offer an actual explanation!DrClaude said:I think that this is completely wrong. The ability to make snowballs is related to the wetness of the snow. Dry snow is not sticky at all, whatever the temperature, and I think the amount of pressure needed to even partially melt it is beyond what you can achieve with your hands. When the snow is wet, no pressure is needed: simply taking a snowball and lightly putting it on fresh snow is enough to make additional stick to it.
There is often a link between the wetness of the snow and temperature: wet snow usually falls when temperatures are close to freezing. But I have often seen dry snow when the temperature is just below freezing. Likewise, old snow that has been on the ground all winter is rarely sticky, whatever the temperature.
Caveat: all this is based on personal experience of having lived nearly all my life in regions where snow is abundant. I have never dug deeper as to what actually makes snow wet and dry.