Much of the southeast is subsiding due to
crustal rebound following the last ice age which compounds any overall ocean rise.
The reasons why the projected sea - level rise at Copenhagen is more severe than at Oslo are complicated, but are primarily related to the effects that we have discussed: Differing rates of
crustal rebound and local gravitational changes at the two cities.
Not exact matches
Alright, I'll give you volcanoes are mostly forcing, we haven't shown a link between
crustal compression and
rebound and activity, yet.