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• W2892015797 abstract "Despite of the fast development of speleothem records, oxygen isotope (δ18O), the main paleoclimatic proxy, remains complicated in climatic interpretation. Continuous cave monitoring is essential for understanding the response of stalagmite oxygen isotope to East Asian Summer Monsoon moisture transportation. We introduce a 7 years (2010–2016) study on oxygen isotope of atmospheric precipitation, cave drips and modern speleothems at Jiguan Cave, central China, located Chinese north–south divide where is sensitive to Asian Monsoon. The monitoring covered a whole ENSO (El Niño Southern Oscillation) cycle, from El Niño in 2010 to La Niña in 2011 and recovered another El Niño in 2015. The precipitation δ18O shows obvious seasonality (negative in summer and positive in winter), but air temperature and rainfall amount are not primary controlling factors. The interannual δ18O of precipitation corresponds with ENSO variability, which means δ18O value is positive during El Niño event and vice versa. We used HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory) model to simulate the moisture transportation for rainy season in El Niño and La Niña years, and found the Pacific contributed over 50% moisture in El Niño years and the Indian Ocean was the predominant oceanic source in La Niña year. There is no seasonality in drips δ18O value, while the response to ENSO variability is evident on interannual scale. The stable negative δ18O of drips compared with precipitation indicate there is a threshold for infiltration, suggesting cave drips are recharged by summer heavy precipitation with light δ18O value, but it’s the mixture of latest and former rainy precipitation that recharge drips in drought, which has been verified by simple infiltration model. We found the modern speleothems were precipitated under nonequilibrium fractionation during drought years, nevertheless, they can record the El Niño related δ18O positive anomaly. Overall, the modern speleothems can receive the precipitation δ18O signal transferred by drips, and our study offers significance for verification of Asian Summer Monsoon driving force and interpretation of stalagmite δ18O." @default.
• W2892015797 created "2018-09-27" @default.
• W2892015797 creator A5009711721 @default.
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• W2892015797 date "2018-11-01" @default.
• W2892015797 modified "2023-10-12" @default.
• W2892015797 title "Potential ENSO effects on the oxygen isotope composition of modern speleothems: Observations from Jiguan Cave, central China" @default.
• W2892015797 cites W1485504984 @default.
• W2892015797 cites W1617734417 @default.
• W2892015797 cites W1820136240 @default.
• W2892015797 cites W1873585162 @default.
• W2892015797 cites W192975001 @default.
• W2892015797 cites W1964179705 @default.
• W2892015797 cites W1964470428 @default.
• W2892015797 cites W1970001087 @default.
• W2892015797 cites W1970658925 @default.
• W2892015797 cites W1977151957 @default.
• W2892015797 cites W1980738681 @default.
• W2892015797 cites W1982002336 @default.
• W2892015797 cites W1996932107 @default.
• W2892015797 cites W2004587064 @default.
• W2892015797 cites W2007463958 @default.
• W2892015797 cites W2009823550 @default.
• W2892015797 cites W2017913935 @default.
• W2892015797 cites W2028972115 @default.
• W2892015797 cites W2032705698 @default.
• W2892015797 cites W2037295081 @default.
• W2892015797 cites W2038031904 @default.
• W2892015797 cites W2039203623 @default.
• W2892015797 cites W2039597298 @default.
• W2892015797 cites W2041095556 @default.
• W2892015797 cites W2041756570 @default.
• W2892015797 cites W2045563285 @default.
• W2892015797 cites W2046373624 @default.
• W2892015797 cites W2047649035 @default.
• W2892015797 cites W2049701477 @default.
• W2892015797 cites W2051201240 @default.
• W2892015797 cites W2052814244 @default.
• W2892015797 cites W2055424629 @default.
• W2892015797 cites W2063009391 @default.
• W2892015797 cites W2063251868 @default.
• W2892015797 cites W2072191315 @default.
• W2892015797 cites W2075145727 @default.
• W2892015797 cites W2079244853 @default.
• W2892015797 cites W2080773859 @default.
• W2892015797 cites W2086192317 @default.
• W2892015797 cites W2086316715 @default.
• W2892015797 cites W2087470097 @default.
• W2892015797 cites W2089325822 @default.
• W2892015797 cites W2093426636 @default.
• W2892015797 cites W2102056066 @default.
• W2892015797 cites W2103561632 @default.
• W2892015797 cites W2104768705 @default.
• W2892015797 cites W2105009853 @default.
• W2892015797 cites W2106700095 @default.
• W2892015797 cites W2106903908 @default.
• W2892015797 cites W2115180998 @default.
• W2892015797 cites W2123407463 @default.
• W2892015797 cites W2129965289 @default.
• W2892015797 cites W2132772276 @default.
• W2892015797 cites W2141643578 @default.
• W2892015797 cites W2146543851 @default.
• W2892015797 cites W2147220992 @default.
• W2892015797 cites W2147526980 @default.
• W2892015797 cites W2148630126 @default.
• W2892015797 cites W2152646374 @default.
• W2892015797 cites W2155905859 @default.
• W2892015797 cites W2156246150 @default.
• W2892015797 cites W2156558129 @default.
• W2892015797 cites W2158003371 @default.
• W2892015797 cites W2162419005 @default.
• W2892015797 cites W2163846204 @default.
• W2892015797 cites W2168619221 @default.
• W2892015797 cites W2168958549 @default.
• W2892015797 cites W2169397092 @default.
• W2892015797 cites W2172293448 @default.
• W2892015797 cites W2208182017 @default.
• W2892015797 cites W2303619177 @default.
• W2892015797 cites W2338996410 @default.
• W2892015797 cites W2464339816 @default.
• W2892015797 cites W2465730685 @default.
• W2892015797 cites W2531618970 @default.
• W2892015797 cites W2570301260 @default.
• W2892015797 cites W2576595946 @default.
• W2892015797 cites W2578390297 @default.
• W2892015797 cites W2618270937 @default.
• W2892015797 cites W2743447327 @default.
• W2892015797 cites W4256468369 @default.
• W2892015797 cites W910256279 @default.
• W2892015797 doi "https://doi.org/10.1016/j.jhydrol.2018.09.015" @default.
• W2892015797 hasPublicationYear "2018" @default.
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