The warm Atlantic water continued to flow into the icy Nordic
seas during the coldest periods of the last Ice Age.
Not exact matches
The researchers found that
during glacial
periods when the atmosphere was
colder and
sea ice was far more extensive, deep ocean waters came to the surface much further north of the Antarctic continent than they do today.
«It is widely thought that
during cold periods of the last Ice Age the warm Atlantic water had stopped its flow into the Nordic
Seas.
The results suggest that warm Atlantic water never ceased to flow into the Nordic
seas during the glacial
period; inflow at the surface
during the Holocene and warm interstadials changed to subsurface and intermediate inflow
during cold stadials.
During the last glacial
period,
sea level dropped 400 feet as water was tied up in ice, and as we have moved out of the
cold glacial
period,
sea level has recovered.
The rate of
sea level rise slowed between 14,000 and 12,000 years ago
during the Younger Dryas
cold period and was succeeded by another surge, «meltwater pulse 1B», 11,500 - 11,000 years ago, when
sea level may have jumped by 28 m according to Fairbanks, although subsequent studies indicate it may have been much less.
If there was actually glaciation
during cold periods, glacial dust might well have blown out to
sea, fertilizing large areas and producing a stronger CO2 pump.
As I said earlier, it would make sense for
sea levels to rise quickly following a
cold period like the LIA - the glaciers that quickly expanded
during that time would just as quickly melt away.
In a 2009 study, the authors used GPS measurement to correct for local vertical movement of the Earth at key tide gages, finding a «global rate of geocentric
sea level rise of 1.61 ± 0.19 mm / yr over the past century» Their study shows no acceleration and no changes in rate
during warm or
cold periods of the last 110 years.
For the
sea star's buffer to work, the ocean water must be sufficiently
cold during periods of high tide.