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浏览/检索结果: 共5条，第1-5条 帮助 限定条件 发表日期：2021     已选(0)清除 条数/页：5101520253035404550556065707580859095100   排序方式：请选择作者升序作者降序题名升序题名降序发表日期升序发表日期降序提交时间升序提交时间降序 Benthic foraminiferal response to orbital-scale variability in primary productivity off the Portuguese margin over the last 1.3 Myr 期刊论文 PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2021, 卷号: 577, 页码: 13 作者:  Guo, Qimei（郭启梅）;  Kim, Jin-Kyoung;  Singh, Arun D.;  Yu, Jing;  Li, Baohua（李保华） 收藏  |  浏览/下载：34/0  |  提交时间：2021/09/07 Benthic foraminiferal turnover  Surface water productivity  Western Iberian margin  Middle-to-late Pleistocene  High-latitude forcing   The Observed North Equatorial Countercurrent in the Far Western Pacific Ocean during the 2014-16 El Nino 期刊论文 JOURNAL OF PHYSICAL OCEANOGRAPHY, 2021, 卷号: 51, 期号: 6, 页码: 2003-2020 作者:  Zhou, Hui;  Liu, Hengchang;  Tan, Shuwen;  Yang, Wenlong;  Li, Yao 收藏  |  浏览/下载：11/0  |  提交时间：2022/04/11 Baroclinic flows  El Nino  ENSO  Instability  Ocean circulation  Ocean dynamics   A three-dimensional gravest empirical mode determined from hydrographic observations in the western equatorial Pacific Ocean 期刊论文 JOURNAL OF MARINE SYSTEMS, 2021, 卷号: 214, 页码: 19 作者:  Liu, Hengchang;  Zhou, Hui;  Yang, Wenlong;  Liu, Xueqi;  Li, Yao 收藏  |  浏览/下载：34/0  |  提交时间：2021/04/21 Nascent NECC  Volume transport  PIES  Non-stationary gravest empirical mode  El Nino   Ocean Circulation in the Challenger Deep Derived From Super-Deep Underwater Glider Observation 期刊论文 Geophysical Research Letters, 2021, 卷号: 48, 期号: 13, 页码: 1-11 作者:  Jiang, Huichang;  Xu HZ(徐洪周);  Vetter, Philip A.;  Xie Q(谢强);  Yu JC(俞建成) 收藏  |  浏览/下载：9/0  |  提交时间：2021/08/03 Deep ocean circulation  the Challenger Deep  underwater glider  volume transport  water properties   Ocean Circulation in the Challenger Deep Derived From Super-Deep Underwater Glider Observation 期刊论文 Geophysical Research Letters, 2021, 卷号: 48, 期号: 13, 页码: e2021GL093169 作者:  Jiang HC(江会常);  Xu HZ(徐洪周);  Vetter Phillip A;  Xie Q(谢强);  Yu JC(俞建成) 收藏  |  浏览/下载：0/0  |  提交时间：2021/12/22 Water property in the Challenger Deep has a three-layer structure  Westward geostrophic flow dominated the Challenger Deep and its core is shallower in the west  Large volume transport of Lower Circumpolar Deep Water (LCDW) about 1.29 Sv passed through the trench area above 7,000 m