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《Arid Zone Research》 2015-04
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Integrated Reconstruction of the Holocene Temperature Series of Qinghai-Tibet Plateau

LI Fan;HOU Guang-liang;E Chong-yi;JIANG Ying-ying;School of Life and Geographic Science,Qinghai Normal University;Physical Geography and Environmental Process Key Laboratory of Qinghai Province,Qinghai Normal University;  
As an important factor affecting the natural environment,climate plays a leading role in the evolution of the natural geographical environment. The Tibetan Plateau is the sensitive area of global climate change. Reconstructing plateau Holocene temperature series not only can recognize the characteristics of the past climate change,but also can evaluate the current global warming trend and predict future climate change.This article selects Plateau 28 locations' fossil sporopollen records and 496 locations' surface soil sporopollen data. We obtain the Holocene temperature series using modern analogy of every point,rebuild Centennial Resolution Holocene temperature integrated series using a single sample area correction method and basing on the integrated idea. The results showed that: Plateau temperature during Holocene can be divided into three phases,the early Holocene( 11. 5- 8. 4 ka B. P.) is the fluctuant warming period,that is to say the temperature rises respectively with fluctuations,and the cold events can be identified during 10. 9,9. 9,9. 2ka B. P. and 8. 9 ka B. P. in this period; The Mid-Holocene( 8. 4- 4. 4 ka B. P.) is the Holocene great warm period,the temperature is higher than the modern in general,megathermal Peak period in 8. 0- 6. 1 ka B. P.,the highest temperature higher than modern 2. 62 ℃ or so,and cold events of the great warm period mainly happened in 8. 2,6. 1,4. 8 ka B. P. or so; The third phase is the late Holocene since 4. 4 ka B. P.,the overall trend is relatively close to the present temperature though the overall temperature fluctuation is also large.Compared with other scholars' reconstructed series,the temperature overall trend basically unanimous; the mainly warm and cold events occurred during the Holocene are basically in corresponding period.
【Fund】: 国家自然科学基金(41161018 41361047);; 青海省自然科学基金(2013-Z-914)
【CateGory Index】: P532
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