A paper published on 4 March in Quaternary Science Reviews reconstructs Arctic temperatures in Kamchatka, USSR over the past 4,500 years and finds the highest reconstructed temperatures were about 3.8°C warmer than modern temperatures. The authors find “the highest reconstructed temperature reaching 16.8 °C between 3700 and 2800 years before the present,” about 3.8°C above “modern temperatures (∼13 °C).”
In addition, the data shows temperatures between 2500 – 1100 [during the Medieval and Roman warming periods] were about 1-2°C above modern temperatures of ~13°C. The paper adds to many other peer-reviewed papers demonstrating that there is nothing unusual, unnatural, or unprecedented regarding modern Arctic temperatures.
|Graph on left side shows reconstructed July temperatures were 1-2°C higher than modern from 2500-1100 years ago [during the Roman and Medieval warming periods], and up to 3.8°C higher than modern from 3700-2800 years ago [during Egyptian and Minoan warming periods]. Second graph from left shows similar changes in Greenland ice core data.|
Late Holocene climate and environmental changes in Kamchatka inferred from the subfossil chironomid record
This study presents a reconstruction of the Late Holocene climate in Kamchatka based on chironomid remains from a 332 cm long composite sediment core recovered from Dvuyurtochnoe Lake (Two-Yurts Lake, TYL) in central Kamchatka. The oldest recovered sediments date to about 4500 cal years BP. Chironomid head capsules from TYL reflect a rich and diverse fauna. An unknown morphotype of Tanytarsini,Tanytarsus type klein, was found in the lake sediments. Our analysis reveals four chironomid assemblage zones reflecting four different climatic periods in the Late Holocene. Between 4500 and 4000 cal years BP, the chironomid composition indicates a high lake level, well-oxygenated lake water conditions andclose to modern temperatures (∼13 °C). From 4000 to 1000 cal years BP, two consecutive warm intervals were recorded, with the highest reconstructed temperature reaching 16.8 °C between 3700 and 2800 cal years BP. Cooling trend, started around 1100 cal years BP led to low temperatures during the last stage of the Holocene.