Not exact matches
Prior to an eruption,
gases — water vapor, carbon dioxide, and sulfur dioxide — bubble out of the magma as it
rises, adding more pressure to the
volcanic system, she explains.
Also, regarding subsea volacanic eruptions — a
volcanic eruption involves release of magma at several thousand degrees C plus superheated
gases — when that hits cold sea water you are going to have a very violent and explosive change of form from lquid water to steam combined with the release of dissolved
gases (mostly CO2)-- I am not sure what laws of Chemistry and Physics you are looking at, but I would suggest that that those bubbles and heated
gases and water will
rise to to the surface very quickly and have a major local effect on any nearby ice.
To that you answer if the temperature ever starts to
rise, due to say
volcanic heat, or upwelling to water's surface, the heat is immediately removed by the power of evaporation as infrared - resonant
gases chug heat straight up through the atmospheric mix to belch it out radiatively at higher altitude; while simultaneously dragging other, non-infrared resonant
gases upward with them, to also dump THEIR heat radiatively, from a higher position than they would have, had the refrigerative cycle not taken place.