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The two-step monsoon changes of the last deglaciation recorded in tropical Maar Lake Huguangyan, southern China 总被引:3,自引:0,他引:3
Wenyuan Wang Jiaqi Liu Dongsheng Liu Tungsheng Liu Ping’an Peng Houyuan Lu Zhaoyan Gu Guoqiang Chu J. Negendank Xiangjun Luo J. Mingram 《科学通报(英文版)》2000,45(16):1529-1532
The concentrations of biogenic silica, total organic carbon, total nitrogen and total hydrogen inferred from the sediments
of tropical Maar Lake Huguangyan, southern China, provide a climate record of the last déglaciation with century resolution.
The records fully demonstrate the existence of the two-step shape of the last déglaciation in tropic East Asia, and they point
out noticeable differences between the low and high latitudes in the Northern Hemisphere. Thus, the Boiling first warming
at the last deglaciation in the low latitude may have preceded that of the high latitude, whereas the cooling of the Younger
Dryas occurred synchronously in the two regions. These results likely suggest that the links between the low and high latitude
climates in the Northern Hemisphere during this period are complexity. 相似文献
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The early Holocene optimum inferred from a hish-resolution pollen record of Husuansyan Maar Lake in southern China 总被引:3,自引:0,他引:3
WANG ShuYun LUE HouYuan LIU JiaQi Joerg F. W. NEGENDANK 《科学通报(英文版)》2007,52(20):2829-2836
A high-resolution pollen record of the past 13000 a from Huguangyan Maar Lake reveals the vegetation and environment changes in southern China during the Holocene. It shows that (i) pollen percentage of trees and shrubs reached 56% during the early Holocene (11600-7800 cal a BP), of which the pollen percentage of tropical trees reached a maximum at 9500-8000 cal a BP, reflecting a hot and wet environment; (ii) during the mid-Holocene (7800-4200 cal a BP), the pollen percentage of montane coniferous trees and herbs increased, while the percentage of tropical-subtropical trees decreased, indicating lower temperature and humidity; (iii) in the late Holocene spanning from 4200 to 350 cal a BP, the pollen percentage of herbs and montane conifer increased significantly, indicating a marked decrease of temperature and humidity. Our pollen data reveal that the time period 9500-8000 cal a BP in southern China represents a climatic optimum for the Holocene characterized by hot and wet conditions. This is consistent with the Holocene optimum found in lower latitude regions globally. We speculate that strong insolation might cause the northward migration of the ITCZ and subtropical summer monsoon front, which resulted in an early Holocene optimum in the Huguangyan area. The dry tendency and climate fluctuations of the middle and late Holocene could be associated with a decrease in solar insolation and frequent ENSO event. 相似文献
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Yancheva G Nowaczyk NR Mingram J Dulski P Schettler G Negendank JF Liu J Sigman DM Peterson LC Haug GH 《Nature》2007,445(7123):74-77
The Asian-Australian monsoon is an important component of the Earth's climate system that influences the societal and economic activity of roughly half the world's population. The past strength of the rain-bearing East Asian summer monsoon can be reconstructed with archives such as cave deposits, but the winter monsoon has no such signature in the hydrological cycle and has thus proved difficult to reconstruct. Here we present high-resolution records of the magnetic properties and the titanium content of the sediments of Lake Huguang Maar in coastal southeast China over the past 16,000 years, which we use as proxies for the strength of the winter monsoon winds. We find evidence for stronger winter monsoon winds before the B?lling-Aller?d warming, during the Younger Dryas episode and during the middle and late Holocene, when cave stalagmites suggest weaker summer monsoons. We conclude that this anticorrelation is best explained by migrations in the intertropical convergence zone. Similar migrations of the intertropical convergence zone have been observed in Central America for the period ad 700 to 900 (refs 4-6), suggesting global climatic changes at that time. From the coincidence in timing, we suggest that these migrations in the tropical rain belt could have contributed to the declines of both the Tang dynasty in China and the Classic Maya in Central America. 相似文献
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末次冰消期热带湖光岩玛珥湖记录的气候事件与GISP2记录的对比 总被引:2,自引:0,他引:2
通过对热带湖光岩玛珥湖沉积物总有机碳、总氮、总氢的分析,揭示了末次冰消期东亚季风发生了多次快速变化的气候事件,并与格陵兰冰芯GISP2记录有较好的对比,但末次冰消期初始转暖湖光岩早于格陵兰,反映了古季风变化的不稳定性以及北半球高低纬度气候连接的复杂性. 相似文献
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湖光岩玛珥湖全新世气候波动的周期性 总被引:31,自引:4,他引:27
对全新世以来湖光岩玛珥湖沉积物干密度高分辨率(10~15a间距)时间序列的能谱分析和滤波分析表明:气候变化存在明显的2930,1140,490, 250和 220a的主周期. 2 930 a周期所对应的3次降温期,其峰值分别发生在7300, 4250和1200 Cal aBP左右.1140a主周期变化,在全新世早期波动幅度最大,到中、晚全新世其幅度逐渐减小,所对应的明显的降温期有7~8次.全新世千年尺度的气候变化,有可能是通过岁差周期(23 070 a)的谐波周期对全球水循环的调整,驱动温盐环流强度的变化,进一步影响了全球气候变化. 相似文献
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Jiaqi Liu Houyuan Lü J. Negendank J. Mingram Xiangjun Luo Wenyuan Wang Guoqiang Chu 《科学通报(英文版)》2000,45(18):1712-1717
There exist five primary periods of 2 930, 1 140, 490, 250 and 220 a in the Holocene climatic variations in the Huguangyan
Maar Lake, according to the energy-spectrum and filter analyses of high-resolution time sequences (10–15 a) of the sediment
dry density. The peak values of the three temperature-decreasing periods with the 2 930 a cycle occur at about 7 300, 4 250
and 1 200 Cal. aBP. There are 7–8 temperature-decreasing periods with the 1 140 a cycle, and the climate fluctuation range
is largest in the early Holocene, and reduces gradually in the middle and late Holocene. The millennial-scale climatic change
in the Holocene may adjust the global water cycle and the thermohaline circulation intensity through the harmonic tones of
the earth’s precession cycle, which in turn influences the global climate change. 相似文献
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