A 200-year annually laminated stalagmite record of precipitation seasonality in southeastern China and its linkages to ENSO and PDO.
A 200-year annually laminated stalagmite record of precipitation seasonality in southeastern China and its linkages to ENSO and PDO.
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中国东南地区200年年层状石笋降水季节记录及其与ENSO和PDO的联系
DOI:
10.1038/s41598-018-30112-6
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发表时间:
2018-08-17
影响因子:
4.6
通讯作者:
Edwards RL
中科院分区:
文献类型:
--
作者:
Zhang H;Cheng H;Spötl C;Cai Y;Sinha A;Tan L;Yi L;Yan H;Kathayat G;Ning Y;Li X;Zhang F;Zhao J;Edwards RL
In southeastern China (SEC), the precipitation amount produced by the East Asian summer monsoon (EASM) is almost equivalent to that during the non-summer monsoon (NSM) period, both of them significantly affecting agriculture and socioeconomy. Here, we present a seasonally-resolved stalagmite δ18O record (δ18Os) for the interval 1810–2009 AD from E’mei cave, Jiangxi Province, SEC. The comparison between δ18Osand instrumental data indicates that the δ18Osvariability is primarily controlled by the precipitation seasonality (i.e., the ratio of EASM/NSM precipitation) modulated by the El Niño/Southern Oscillation (ENSO) on interannual to interdecadal timescales. Higher (lower) δ18Osvalues thereby correspond to lower (higher) EASM/NSM ratios associated with El Niño (La Niña) events. Significant correlations with ENSO and the Pacific Decadal Oscillation (PDO) indicate that the precipitation seasonality in SEC is remarkably influenced by ocean-atmosphere interactions, with lower (higher) EASM/NSM ratios during warm (cold) phases of ENSO/PDO. The progressive increase in δ18Ossince 2005 AD may reflect a strengthening of the central Pacific El Niño under continued anthropogenic global warming. The relationship between seasonal precipitation and δ18Oswith ENSO/PDO requires further studies.
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影响因子:
5.2
作者:
Gong, DY;Ho, CH
通讯作者:
Ho, CH
影响因子:
4.4
作者:
Schulz, M;Mudelsee, M
通讯作者:
Mudelsee, M
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作者:
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通讯作者:
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作者:
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通讯作者:
Kathleen R. Johnson
影响因子:
5.3
作者:
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通讯作者:
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