But again the «models» estimate includes an observed ice sheet mass loss term of 0.41 mm / year
whereas ice sheet models give a mass gain of 0.1 mm / year for this period; considering this, observed rise is again 50 % faster than the best model estimate for this period.
Our estimated sea levels have reached +5 to 10 m above the present sea level during recent interglacial periods that were barely warmer than the Holocene,
whereas the ice sheet model yields maxima at most approximately 1 m above the current sea level.
Not exact matches
In LGM simulations land albedo changes are prescribed (at least in regards to
ice sheets and altered topography due to sea level; there are feedback land albedo changes) so are a forcing,
whereas sea
ice is determined interactively by the
model climate, so is a feedback in this framework.