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In page Subboreal:
"The climate was generally drier and slightly cooler (by about 0.1 °C) than in the preceding Atlantic but still warmer than during the 20th century. The temperatures were 0.7 °C higher than during the following Subatlantic. Consequently, in Scandinavia the lower limit of glaciers was 100 to 200 m higher than during the Subatlantic.[1] On the whole, the oscillating temperatures slightly receded in the course of the Subboreal by about 0.3 °C.[citation needed]
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