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Here’s a recently published paper on sea surface temperatures 3 million years ago when the Arctic was seasonally ice free:
http://micropress.org/stratigraphy/papers/Stratigraphy_6_4_265-275.pdf
The paper presents some interesting data. The most northern location sampled was found to be 18C warmer during the summer. That's huge! It was found just off the coast of Spitsbergen; a chain of island that was (until a few years ago) encrusted in ice most of the year. In contrast, temperatures at tropical sites were found to be similar to those of today.
They also found evidence of significant warming off the coast of California and western South America compared to less warming further off shore. So, the global warming of that time was not at all uniform.
Note; at the current rate of sea ice retreat and thinning, the Arctic may be seasonally ice free by 2040. As such, this study provides a possible analog for our future climate conditions. CO2 levels during that time period were close or just slightly higher than current levels.
http://micropress.org/stratigraphy/papers/Stratigraphy_6_4_265-275.pdf
The paper presents some interesting data. The most northern location sampled was found to be 18C warmer during the summer. That's huge! It was found just off the coast of Spitsbergen; a chain of island that was (until a few years ago) encrusted in ice most of the year. In contrast, temperatures at tropical sites were found to be similar to those of today.
They also found evidence of significant warming off the coast of California and western South America compared to less warming further off shore. So, the global warming of that time was not at all uniform.
Note; at the current rate of sea ice retreat and thinning, the Arctic may be seasonally ice free by 2040. As such, this study provides a possible analog for our future climate conditions. CO2 levels during that time period were close or just slightly higher than current levels.
ABSTRACT: The most recent geologic interval characterized by warm temperatures similar to those projected for the end of this century occurred about 3.3 to 3.0 Ma, during the mid-Piacenzian Age of the Pliocene Epoch. Climate reconstructions of this warm period are integral to both understanding past warm climate equilibria and to predicting responses to today’s transient climate. The Arctic Ocean is of particular interest because in this region climate proxies are rare, and climate models struggle to predict climate sensitivity and the response of sea ice. In order to provide the first quantitative climate data from this region during this interval, sea surface temperatures (SST) were estimated from Ocean Drilling Program Sites 907 and 909 in the Nordic Seas and from Site 911 in the Arctic Ocean based on Mg/Ca of Neogloboquadrina pachyderma (sin) and alkenone unsaturation indices. Evidence of much warmer than modern conditions in the Arctic Ocean during the mid-Piacenzian with temperatures as high as 18°C is presented. In addition, SST anomalies (mid-Piacenzian minus modern) increase with latitude across the North Atlantic and into the Arctic, extending and confirming a reduced mid-Piacenzian pole-to-equator temperature gradient. The agreement between proxies and with previously documented qualitative assessments of intense warming in this region corroborate a poleward transport of heat and an at least seasonally ice-free Arctic, conditions that may serve as a possible analog to future climate if the current rate of Arctic sea-ice reduction continues.