Seems to be no doubt in the minds of these research scientists as to what the future holds.
http://www.polarresearch.net/index.php/polar/article/download/6172/6851
Abstract
Sediment cores from the Norwegian Sea were studied to evaluate interglacial
climate conditions of the marine isotope stage 5e (MIS 5e). Using planktic
forminiferal assemblages as the core method, a detailed picture of the evolution
of surface water conditions was derived. According to our age model, a steplike
deglaciation of the Saalian ice sheets is noted between ca. 135 and
124.5 Kya, but the deglaciation shows little response with regard to surface
ocean warming. From then on, the rapidly increasing abundance of subpolar
forminifers, concomitant with decreasing iceberg indicators, provides evidence
for the development of interglacial conditions sensu stricto (5e-ss), a period that
lasted for about 9 Ky. As interpreted from the foraminiferal records, and
supported by the other proxies, this interval of 5e-ss was in two parts: showing
an early warm phase, but with a fresher, i.e., lower salinity, water mass, and a
subsequent cooling phase that lasted until ca. 118.5 Kya. After this time, the
climatic optimum with the most intense advection of Atlantic surface water
masses occurred until ca. 116 Kya. A rapid transition with two notable climatic
perturbations is observed subsequently during the glacial inception. Overall,
the peak warmth of the last interglacial period occurred relatively late after
deglaciation, and at no time did it reach the high warmth level of the early
Holocene.
This finding must be considered when using the last interglacial
situation as an analogue model for enhanced meridional transfer of ocean heat
to the Arctic, with the prospect of a future warmer climate.