Articles | Volume 10, issue 3
https://doi.org/10.5194/cp-10-1211-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-10-1211-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
24 Jun 2014
Research article |
| 24 Jun 2014
Stalagmite-inferred variability of the Asian summer monsoon during the penultimate glacial–interglacial period
Key Laboratory of Eco-environments in Three Gorges Reservoir Region, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi'an 710075, China
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC
C.-C. Shen
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC
L.-J. Huang
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC
X.-Y. Jiang
College of Geographical Science, Fujian Normal University, Fuzhou 350007, China
X.-L. Yang
Key Laboratory of Eco-environments in Three Gorges Reservoir Region, Ministry of Education, School of Geographical Sciences, Southwest University, Chongqing 400715, China
H.-S. Mii
Department of Earth Sciences, National Taiwan Normal University, Taipei 11677, Taiwan, ROC
S.-Y. Lee
Research Center for Environmental Changes, Academia Sinica, Taipei 11529, Taiwan, ROC
L. Lo
High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei 10617, Taiwan, ROC
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Permafrost in Eurasian continent is extremely sensitive to global climate change. We used the data of 15 stations from the Global Network of Isotope in Precipitation (GNIP) and proposed that the δ18OP was correlated with local temperature on the monthly and seasonal timescales. However, on the annual timescale, except for
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A coral reconstruction of past climate shows changes in the seasonal cycle of sea surface temperature in the SE tropical Indian Ocean. An enhanced seasonal cycle suggests that the tropical rainfall belt shifted northwards between 1855–1917. We explain this with greater warming in the NE Indian Ocean relative to the SE, which strengthens surface winds and coastal upwelling, leading to greater cooling in the eastern Indian Ocean south of the Equator.
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The oxygen isotopic ratio of water in fluid inclusions in speleothems is an important proxy for the changes in past hydroclimate and temperatures. This isotopic ratio, however, may be affected by isotopic exchange between the water and the host calcite. Here we evaluate this exchange reaction based on a laboratory experiment. We demonstrated that the exchange was detectable but not significant for temperature reconstruction, likely because the reaction occurred only with a thin calcite layer.
Tao Wang, Ting-Yong LI, Jian Zhang, Yao Wu, Chao-Jun Chen, Ran Huang, Jun-Yun Li, and Si-Ya Xiao
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Permafrost in Eurasian continent is extremely sensitive to global climate change. We used the data of 15 stations from the Global Network of Isotope in Precipitation (GNIP) and proposed that the δ18OP was correlated with local temperature on the monthly and seasonal timescales. However, on the annual timescale, except for
temperature effect, δ18OP also reflects the change of water vapor source dominated by Eurasian Zonal Circulation (EZC) and North Atlantic Oscillation (NAO).
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Clim. Past Discuss., https://doi.org/10.5194/cp-2017-144, https://doi.org/10.5194/cp-2017-144, 2017
Manuscript not accepted for further review
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Recent Southern Hemisphere (SH) atmospheric circulation, predominantly driven by stratospheric ozone depletion over Antarctica, has caused changes in climate across the extratropics. We present evidence that the Brazilian coast may have been impacted from both wind and sea surface temperature changes derived from this process. Skeleton analysis of massive coral species living in shallow waters off Brazil are very sensitive to air–sea interactions and seem to record this process.
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Clim. Past, 12, 871–881, https://doi.org/10.5194/cp-12-871-2016, https://doi.org/10.5194/cp-12-871-2016, 2016
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The upper part of stalagmite ky1 (from top to 42.769 mm depth), consisting of 678 laminae, was collected from a cave in northern China, located in the East Asia monsoon area. The time of deposition ranges from AD 1217±20 to 1894±20. The analysis shows that both the variations in the thickness of the laminae themselves and the fluctuating degree of variation in the thickness of the laminae of stalagmite ky1 have obviously staged characteristics and synchronized with climate.
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1. We have reconstructed new meridional thermal and precipitation stacked records in the Indo-Pacific Warm Pool (IPWP) during the last termination.
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C. R. Maupin, J. W. Partin, C.-C. Shen, T. M. Quinn, K. Lin, F. W. Taylor, J. L. Banner, K. Thirumalai, and D. J. Sinclair
Clim. Past, 10, 1319–1332, https://doi.org/10.5194/cp-10-1319-2014, https://doi.org/10.5194/cp-10-1319-2014, 2014
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Subject: Teleconnections | Archive: Terrestrial Archives | Timescale: Pleistocene
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Volcanic ash layers in Lake El'gygytgyn: eight new regionally significant chronostratigraphic markers for western Beringia
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B. Wagner, M. J. Leng, T. Wilke, A. Böhm, K. Panagiotopoulos, H. Vogel, J. H. Lacey, G. Zanchetta, and R. Sulpizio
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