georgeob1 wrote:Foxfyre wrote:
Okay, for us thermodynamically challenged, could you put that into layman's terms as to what happens to the heat that is released when water freezes or becomes colder?
It is probably more accurate and intuitively satisfying to say that melting ice requires that heat be transferred to it from its surroundings. Heat flows only in the presence of a difference in the temperatures of source and sink. Heat can be transferred by (1) Conduction from objects in direct contact (this is basically the transfer of energy from molecule to molecule in collisions); (2) Convection from a flowing stream of liquid or gas in direct contact (the flow in effect transports heat to the boundary); Radiation, which involves the flow of photons from the hotter object to a cooler one (it is the heat you feel when you put your hand a few inches above a lighted stove, or near an incandescent light bulb -- broiled foods are cooked by radiation as are those in a microwave oven.)
So the melting of the Antarctic ice requires that it be in direct contact with air or water at a temperature above the local freezing point. Heat flows from the warmer air or water to the ice during the melting. As a result the air or water cools. Generally there are convective flows of the air and water around the ice which effectively replenish the thermal energy in the air/water in contact with the ice. If an equilibrium is reached the ice stops melting.
In dry, clear air with intense sunlight ice can sublimate directly from a crystalline state to vapor due to intense radiation heat transfer. You likely see this in the Rocky Mountain area quite frequently.
Okay, I almost understood that. (You have a way to go to explain it to the really challenged on this stuff though.
)
But okay. I recently asked a question related to a NASA graphic showing that the large land mass of Anarctica was getting colder and the ice thickening--while the perimeter of Anarctica was shown as getting somewhat warmer.
Now when I was growing up amongst fruit and vegetable farmers, they sometimes used large tubs of water or ran water into the irrigation ditches just before a predicted freeze. The theory was that the water would emit just enough heat as it chilled and froze to keep the tender blossoms from being destroyed.
Now my question was that if the vast interior of Anarctica is cooling, doesn't the heat that was there have to go somewhere? And would the logical place for it to go be around the perimeter which could explain temporarily slightly higher temperatures? And if this is so, then could this be an alternate explanation and the whole phenomenon does not necessarily have to be caused by global warming?
So far nobody has wanted to answer the question, though I have received a good deal of grief for asking it.
(And yes, on some days the mountains and rocks absolutely glow about sundown as they give up the heat they absorbed during the day. It's one of my favorite things. And the ground fog phenomenon can be stunning as well.)