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