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Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea

机译：基于东海北部氧同位素质量平衡的长江（长江）淡水通量重建推断全新世东亚夏季风降水变化

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Y. Kubota; R. Tada; K. Kimoto;
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1. Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea [J] . Y.Kubota, R.Tada, K.Kimoto Climate of the past . 2015,第2期

机译：基于东海北部氧同位素质量平衡的长江（长江）淡水通量重建推算出全新世期间东亚夏季风降水的变化
2. Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea [J] . Kubota Y., Tada R., Kimoto K. Climate of the Past Discussions . 2015,第2期

机译：基于东海北部氧同位素质量平衡的长江（长江）淡水通量重建推算出全新世期间东亚夏季风降水的变化
3. Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea [J] . Kubota Y., Tada R., Kimoto K. Climate of the past . 2015,第2期

机译：基于东海北部氧同位素质量平衡的长江（长江）淡水通量重建推算出全新世期间东亚夏季风降水的变化
4. Verifying a New Proxy of the Holocene East Asian Winter Monsoon-Grain Size of Mud on the Inner Shelf of the East China Sea [C] . Xiao Shangbin, Tian Fang, Zhang Guodong, . 2007

机译：验证东海内层全新世东亚冬季季风粒度的新替代物
5. East Asian summer monsoon precipitation systems: Rainfall characteristics, storm morphologies and convective properties. [D] . Xu, Weixin. 2011

机译：东亚夏季风降水系统：降雨特征，风暴形态和对流性质。
6. East Asian Monsoon Signals Reflected in Temperature and Precipitation Changes over the Past 300 Years in the Middle and Lower Reaches of the Yangtze River [O] . Zhixin Hao, Di Sun, Jingyun Zheng -1

机译：长江中下游近300年气温和降水变化的东亚季风信号
7. Kubota, Y., Tada, R. & Kimoto, K. 2015. Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea. Climate of the Past, 11, 265–281, doi: 10.5194/cp-11-265-2015. [O] . 久保田, 好美, 多田, 隆治, 木元, 克典, 2015

机译：Y. Kubota，Y.，Tada，R。和Kimoto，K.，2015。基于东部北部氧同位素质量平衡的长江（长江）淡水通量重建推导的全新世期间东亚夏季风降水的变化。中国海。过去的气候，11，265–281，doi：10.5194 / cp-11-265-2015。
8. Discharge of the Changjiang (Yangtze River) into the East China Sea [R] . Beardsley, R. C., Limeburner, R., Yu, H., 1985

机译：长江（长江）流入东海

Changes in East Asian summer monsoon precipitation during the Holocene deduced from a freshwater flux reconstruction of the Changjiang (Yangtze River) based on the oxygen isotope mass balance in the northern East China Sea

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