机译:自上次冰河最高峰以来中国北方沙漠的水汽重构,及其对东亚夏季风的影响
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China,University of Chinese Academy of Sciences, Beijing, 100049, China,Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China;
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China;
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China;
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China,University of Chinese Academy of Sciences, Beijing, 100049, China;
Physical Geography, Faculty of Sciences, University of Novi Sad, Novi Sad, 21000, Serbia;
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China;
East Asian summer monsoon; effective moisture; dune activity; vegetation; Last Glacial Maximum; sea level;
机译:自上次冰河最高峰以来重建南海南部高水柱结构:对东亚冬季风发展的启示
机译:东亚夏季风保持中国西南戈壁沙漠的夏季相对湿度:来自年轮δ〜(18)O的证据
机译:东亚夏季季风湿度维持夏季戈壁沙漠的夏季相对湿度:来自δ〜(18)o的δ〜(18)o的证据
机译:过去539YR东亚夏季季风和干旱洪水分布的进化
机译:温暖气候对亚洲夏季季风影响的大气循环影响
机译:中国洞穴δ18O记录不代表东亚北部夏季风
机译:自上次冰河最高峰以来重建南中国海南部高水柱结构:对东亚冬季风发展的启示