Indeed, ice has more volume. And that extra volume is the thing sticking up above the water surface. Take 1 kg (1L) of water, freeze it (roughly 1.1L). The ice cube will float, but also displace 1 kg (1L) of water. This is one version to weight things less dense than water. If an object becomes completely submerged (by weight or force) the you get its volume, by the displacement of water.
Melting completely submerged ice would lower the water level, but it would require something to keep the ice from floating up.
The worser scenarios are about 0.5-2 meters in a century.
Antartica contains ice equivalent to about a 60 meter water rise.
Greenland about 7 meters.
And yes, melting all of it would take thousands of years.
Land bound or bottom frozen (with abundant ice above sea level) regions are those that increases the sea level. It's the same principle that made the water level more than 100 meters lower than today during, the ice ages.
And for the fun of it. Fragony, the only relevance the depth has, is that increased water temperature increases the volume of water. It's very minor, but on 4 km (estimated average water depth) of water it makes a difference. Going from 4 C water to 30 C would cause a sea level rise of 17 meters. I doubt this factor is going to matter much normally (an average sea temp of 30 C is proably a half desert Earth or something like that), but it exists.
Bookmarks