5篇
您的检索式：作者名="SPRINTALL Janet"
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| 1 | Review on observational studies of western tropical Pacific Ocean circulation and climate显示文摘The Western Tropical Pacific(WTP) Ocean holds the largest area of warm water(>28℃) in the world ocean referred to as the Western Pacific Warm Pool(WPWP),which modulates the regional and global climate through strong atmospheric convection and its variability.The WTP is unique in terms of its complex 3-D ocean circulation system and intensive multiscale variability,making it crucial in the water and energy cycle of the global ocean.Great advances have been made in understanding the complexity of the WTP ocean circulation and associated climate impact by the international scientific community since the 1960 s through field experiments.In this study,we review the evolving insight to the 3-D structure and multi-scale variability of the ocean circulation in the WTP and their climatic impacts based on in-situ ocean observations in the past decades,with emphasis on the achievements since 2000.The challenges and open que stions remaining are reviewed as well as future plan for international study of the WTP ocean circulation and climate. | HU Dunxin WANG Fan SPRINTALL Janet WU Lixin RISER Stephen CRAVATTE Sophie GORDON Arnold ZHANG Linlin CHEN Dake ZHOU Hui ANDO Kentaro WANG Jianing LEE Jae-Hak HU Shijian WANG Jing ZHANG Dongxiao FENG Junqiao LIU Lingling VILLANOY Cesar KALUWIN Chalapan QU Tangdong MA Yixin | 2020 | Journal of Oceanology and Limnology2020，38，4： | 3 |
| 2 | The intermediate water in the Philippine Sea显示文摘The dimensional and temporal distribution of Antarctic Intermediate Water(AAIW)and North Pacifi c Intermediate Water(NPIW)in the Philippine Sea were explored using Argo profi les and gridded Argo data.As the salinity minimum of intermediate water from mid-high latitude of the southern and northern hemisphere of the Pacifi c Ocean,the properties of AAIW and NPIW merge at about 10°N with diff erent properties in the Philippine Sea.The core of AAIW is located below 600 dbar with potential density of 27≤σθ≤27.3 kg/m 3 and salinity of 34.5≤S≤34.55.The core of NPIW is located between 300–700 dbar with potential density of 26.2≤σθ≤27 kg/m 3 and salinity of 34≤S≤34.4.The volume of AAIW and NPIW during January 2004 to December 2017 is negatively correlated.The time series of AAIW and NPIW is dominated by signifi cant periods of 6 and 8 months,respectively.The variations of AAIW and NPIW are mainly aff ected by volume transport through a 130°E section by the North Equatorial Current(NEC)and North Equatorial Undercurrent(NEUC). | ZANG Nan WANG Fan SPRINTALL Janet | 2020 | Journal of Oceanology and Limnology2020，38，5： | 1 |
| 3 | Location of the Antarctic Polar Front from AMSR-E Satellite Sea Surface 显示文摘 | Shenfu Dong Janet Sprintall Sarah T Gille | 2006 | Journal of Physical Oceanography2006，36，9： | 1 |
| 4 | Surface inflow into the South China Sea through the Luzon Strait in winter显示文摘我们在冬季季风期间学习了自台湾东面的菲律宾海流向日本的暖流侵入的驱动力进华南海(SCS ) ,用进入通过来自菲律宾的海的 Balintany 和 Babuyan 隧道的吕宋岛海峡(LS ) 的追踪卫星的流浪者。没有一个重要变化,在冬季通过 Babuyan 隧道的大多数流浪者在速度进入了内部 SCS。然而,通过 Balintany 隧道的流浪者的一半在 30 cm/s 进入了 SCS,它比他们什么时候进入 LS 快。另外的一半继续移动进自台湾东面的菲律宾海流向日本的暖流向西北、对北方太平洋回来。量的分析,使用的表面 climatological 风和海出现高度异例(SSHa ) 数据通过 Balintany 隧道在在二条隧道和他们的加速之间的流浪者的速度向两个解释了差别。结果建议海的积极南方的坡度出现在吕宋岛海峡的高度,由东北季风,以及 Ekman 流动驾驶的海水的连环相撞引起了,通过 Babuyan 和 Balintany 隧道贡献自台湾东面的菲律宾海流向日本的暖流侵入进 SCS。前者可以是主要驱动力。 | 郭景松 陈显尧 Janet SPRINTALL 郭炳火 乔方利 袁业立 | 2012 | Chinese Journal of Oceanology and Limnology2012，30，1： | 1 |
| 5 | Location of the Antarctic Polar Front from AMSR-E Satellite Sea Surface 显示文摘 | Shenfu Dong Janet Sprintall Sarah T Gille | 2006 | Journal of Physical Oceanography2006，36，9： | 1 |
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