机译:基于树轮的山岳降水重建。中国兴隆,始建于1679年
The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China,Department of Environmental Science and Technology, School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an 710049, China;
The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China,Graduate University of the Chinese Academy of Sciences, Beijing 100049, China;
The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China,Graduate University of the Chinese Academy of Sciences, Beijing 100049, China;
The State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China,Graduate University of the Chinese Academy of Sciences, Beijing 100049, China;
Department of Environmental Science and Technology, School of Human Settlements and Civil Engineering, Xi'an Jiaotong University, Xi'an 710049, China;
机译:中国西北地区基于年轮的降水重建与印度洋和太平洋海面温度之间的协变性
机译:中国西北地区基于年轮的降水重建与印度洋和太平洋海面温度之间的协变性
机译:基于2917年的树木圈改性的布尔汉布纳MTS。,中国东南部的南德兰盆地
机译:MT的雾气和沉淀化学1997年4月至1998年3月在神户的六甲
机译:基于树木年轮的加拿大南部山脉降水重建
机译:青山青海云杉树环宽度的温度重建。西北地区东大地区及其与大规模气候强迫的关系
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。