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Carbon Dioxide and Earth's Future Pursuing the ... - Magazooms

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www.co2science.org<br />

P a g e | 9<br />

The distribution of studies that allow one to determine whe<strong>the</strong>r peak Medieval Warm Period<br />

temperatures were warmer than (red), equivalent to (green), or cooler than (blue), peak<br />

Current Warm Period temperatures. These studies do not include those of <strong>the</strong> preceding<br />

figure, <strong>the</strong> blue ones of which should be added to <strong>the</strong> blue ones of this figure, <strong>and</strong> <strong>the</strong> red<br />

ones of which should be added to <strong>the</strong> red ones of this figure, if true totals of <strong>the</strong>se two result<br />

categories are desired.<br />

The story told by <strong>the</strong> two figures above seems pretty clear: <strong>the</strong> peak warmth of <strong>the</strong> MWP was<br />

typically, but not universally, greater than <strong>the</strong> peak warmth of <strong>the</strong> CWP has been to date. And<br />

that earlier period of greater warmth occurred at a time when <strong>the</strong> atmosphere’s CO2<br />

concentration was fully 100 ppm less than it is today, indicative of <strong>the</strong> fact that <strong>the</strong> earth has<br />

experienced equivalent or warmer temperatures than those of <strong>the</strong> present when <strong>the</strong>re was<br />

much less CO2 in <strong>the</strong> air, which suggests that whatever was responsible for <strong>the</strong> greater warmth<br />

of <strong>the</strong> MWP could easily be responsible for <strong>the</strong> lesser warmth of <strong>the</strong> CWP.<br />

In discussing one final large-scale study that did not mix apples <strong>and</strong> oranges between its early<br />

<strong>and</strong> later stages, Ljungqvist (2010) developed a 2000-year temperature history of <strong>the</strong> extratropical<br />

portion of <strong>the</strong> Nor<strong>the</strong>rn Hemisphere (i.e., that part covering <strong>the</strong> latitudinal range 30-<br />

90°N) based on 30 temperature-sensitive proxy records with annual to multi-decadal<br />

resolution, including two historical documentary records, three marine sediment records, five<br />

lake sediment records, three speleo<strong>the</strong>m δ 18 O records, two ice-core δ 18 O records, four varved<br />

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