@Olivier5,
Olivier5 wrote:
Quote:The question is how high?
Current estimates circle around 3 or 4 feet by the end of this century. It won't stop there, though. The estimated maximum sea level rise, assuming all ice on land melts into the sea, is over 200 ft. Might take us a few centuries to get there.
Also consider that as sea-level rises, the shallow coastal waters are the warmest part of the ocean, so water evaporates there the fastest.
The geological processes that keep the oceans deep and the land steep are incredibly slow. If weathering and erosion processes outpace them, the build up of sediments mean more shallow water, which means more/faster evaporation.
A fast-churning water-cycle at a global scale will accelerate the weathering and erosion of mountains and land, which will intensify the feedback loop of sea-level rise; although the actual rise of liquid water measurable as sea-level will be tempered by atmospheric water-volume rise because more water will go up and not come down.
With overall more H2O and CO2 cycling between the surface and atmosphere, we can expect faster weathering/erosion along with the other effects of greater heat-blanketing.
It helps to look at the whole process in terms of the final state of eventual total submersion of all land underwater. This final 'water world' state the Earth is progressing toward can take more or less time depending on what kinds of stable energy-patterns are established and sustained.
It is conceivable that energy-patterns could be established and sustained that would allow the energy-patterns that drive the tectonic shifts and mountain-range growth to outpace the weathering/erosion that raise sea-levels.
It is also conceivable that we will continue to convert potential energy stored within the planetary system into kinetic energy at a pace faster than it can be re-potentiated as new stored energy. In that case, weathering/erosion will continue to forge a path ahead of the slow geological processes that build up new land and deepen oceans, which keep the oceans colder, mountains higher, and permafrost colder and thus more reflective of sunlight.