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An extended Arctic proxy temperature database for the past 2,000 years.
The figure, discussed in a much quoted email from Jones in which he used a "trick" to "hide the decline", spliced together proxy temperature data and instrument data.
However, another important climate driver, volcanic forcing has generally been underestimated prior to the past 2,500 years partly owing to the lack of proper proxy temperature records.
Over hotter surfaces, the background infrared test is needed for the proxy temperature reading to be accurate.
Second, time dependent glacier simulations forced by a nearby proxy temperature record derived from chironomids are used to assess the fit with the glacial geomorphic record.
Most of proxy temperature records are from tree-ring measurements, but additional evidence comes from glacier ice, speleothems [stalagmites, stalactites and related mineral formations], corals and lake sediments.
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In Section 3, we review the seasonal and vertical distribution patterns of each proxy-related producer in the water column to examine what the proxy temperatures represent.
They then combine proxy temperatures from several sites to infer an average global or regional temperature, giving some proxies more weight because they show a stronger relation to temperature.
Overall, comparisons of proxy temperatures between the two periods suggest that SSTs during the LGM were lower than those during the late Holocene.
The February assemblage SSTs were lower than the alkenone- and Mg/Ca-based temperatures during the late Holocene but close to the two other proxy temperatures during the LGM.
However, the February foraminiferal assemblage-based SSTs were 2.7 3.7 °C cooler than the alkenone- and Mg/Ca-based temperature estimates during the late Holocene, although foraminiferal assemblage-based SSTs were consistent with other proxy temperatures during the LGM.
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CEO of Professional Science Editing for Scientists @ prosciediting.com