I checked the temp rise from a graph of central Greenland temperatures and my eyeball rise was 0.7C for the last 100 years. which is similar the the rise in hadcrut3.
Link appears dead.
I have my doubts. See:
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Conclusions and perspectives
The paleolimnological study of this northern Southampton Island lake provides information and extends the spatial understanding of Northern Hemisphere climatic events (Medieval Warm Period and Little Ice Age) in the Foxe Basin region. Both chironomid-based August air temperature inferences and sedimentological assemblages suggest that Southampton Island was affected by a regional warming between cal yr AD 1160?1360 and a regional cooling between cal yr AD 1360? 1700. These results compare well with both archaeological studies made on Southampton Island and paleoclimatic studies conducted on the southern part of Baffin Island. In the present study, the information extracted based on the biological indicators (chironomids) was supported by a large range of sedimentological analyses. Such results confirm the importance of including sedimentological proxies when interpreting chironomid analysis as they provided an extended overview of the past hydrological and geochemical status of the lake which has affected its biological community. The large number of lakes covering the arctic landscape provides a real opportunity to improve our knowledge of past natural climates in still poorly studied arctic regions and develop new frameworks for the evolution of such freshwater ecosystems under the now called ?Anthropocene.?
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Figure 1 shows the summer (June, July August) average temperature from the weather station located at Clyde, Northwest Territory, which is located on Baffin Island very near the site of the lake. There is no trend here from 1943 to 2008, the period of available data. The most remarkable events are a couple of very cold summers and one very warm summer?all in the 1970s. Summers in the most recent decade are little different than summers in the 1950s?hardly a sign that human-caused ?global warming? has made environmental conditions there particularly unique.
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No but the Old Kingdom was during the climate optimum which was noticeably warmer than now and Egypt more fertile.
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By 5000 to 3000 BC average global temperatures reached their maximum level during the Holocene and were 1 to 2 degrees Celsius warmer than they are today. Climatologists call this period either the Climatic Optimum or the Holocene Optimum.
During the climatic optimum many of the Earth's great ancient civilizations began and flourished. In Africa, the Nile River had three times its present volume, indicating a much larger tropical region. 6,000 years ago the Sahara was far more fertile than today and supported large herds of animals, as evidenced by the Tassili N'Ajjer frescoes of Algeria (right).
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SNIP