Not exact matches
While the ice build up is
likely slow due to
decreasing temps, the eventual increasing temperature begins to
melt massive ice dams slowly at first with little change down stream.
However, this situation ended when the freshwater flux from ice - sheet
melting decreased and a newly enhanced thermohaline circulation in the Atlantic was
likely to have extended the interglacial warmth during the latter part of the Last Interglacial.
[Quite the opposite effect may be the case: as the area of ice
decreases (as it has been since the last ice age), so it is
likely that the quantity of ice being
melted by the ocean each year
decreases, this would reduce a cooling effect on the ocean (entirely independent of AGW obviously) possible causing lower level temperature rises]
This most
likely is due the fact that we have come to the end of the LIA —
melting has
decreased substantially.