共被期刊论文引用了3次
您的检索式：您选中1篇文献正在查看引证文献汇总
|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | 南极普里兹湾及其邻近海域水团研究显示文摘普里兹湾及其邻近海域是中国南大洋调查研究的传统优势海域与重点区域。围绕夏季表层水、冬季水、陆架水、绕极深层水、南极底层水、普里兹湾底层水、冰架水等研究海区主要水团的特征和分布,总结了前人在南极普里兹湾及其邻近海域基于调查资料开展的水团研究中所取得的成果。研究表明,前人在对陆架水的示性指标界定上,将陆架水是否区分为高盐陆架水和低盐陆架水存在较大争议,在高盐陆架水和普里兹湾底层水的定义上存在重叠;目前尚没有证据表明绕极深层水向南可以伸展到普里兹湾的陆架区域,也没有发现在普里兹湾附近海域生成南极底层水的直接证据。 | 陈红霞 林丽娜 史久新 | 2014 | 海洋学报2014，36，7： | 10 |
| 2 | Progress of Chinese research in physical oceanography of the Southern Ocean显示文摘Oceanographic surveying has been one of the key missions of the Chinese National Antarctic Research Expedition since 1984. Using the field data obtained in these surveys and the results from remote sensing and numerical models, Chinese physical oceanographers have investigated the water masses, fronts and circulation patterns in the Southern Ocean. The results of nearly 30 years of research are summarized in this paper. Most oceanographic observations by Chinese researchers have been conducted in Prydz Bay and the adjacent seas. CTD (Conductivity Temperature and Depth) data, collected during the past 20 years, have been applied to study several features of the water masses in this region: The spatial variation of warm summer surface water, the northward extension of shelf water, the flow of ice shelf water from the cavity beneath the Amery Ice Shelf, the upwelling of the Circumpolar Deep Water, and the formation of the Antarctic Bottom Water. The circulation and its dynamic factors have been analyzed with dynamic heights calculated from CTD data as well as by numerical models. The structure and strength of the fronts in the southeast Indian Ocean and the Drake Passage were investigated with underway XBT/XCTD (Expendable Bathythermograph/Expendable CTD) and ADCP (Acoustic Doppler Current Profiler) data. Their interannual variations have been determined and the factors of influence, especially the atmospheric forcing and mesoscale oceanic processes, were studied using remote sensing data. The dynamic mechanism of the Antarctic Circumpolar Current (ACC) was analyzed by theoretical models. The transport and pattern of the ACC have been well reproduced by coupled sea ice-ocean models. Additional details of ACC variability were identified based on satellite altimeter data. The response of the ACC to climate change was studied using reanalysis data. Prospects for future research are presented at the end of this paper. | SHI Jiuxin DONG Zhaoqian CHEN Hongxia | 2013 | Advances in Polar Science2013，24，2： | 5 |
| 3 | 2013年夏季普里兹湾水团分析显示文摘为了解南大洋水团的分布特征并进一步为渔业生产提供信息参考,本文采用雪龙号第29次南极考察CTD数据,通过定性综合分析法、浓度混合分析法以及聚类分析法对2013年夏季普里兹湾水团进行了分析。研究结果表明,2013年夏季普里兹湾共存在6个水团,分别为夏季表层水、冬季陆架混合水、夏季冬季混合水、冰架水、绕极深层水和南极底层水。其中夏季表层水位于普里兹湾东北海域,只占薄薄的一层;冰架水向北可延伸至66°48′S;绕极深层水以及南极底层水在大陆坡处都存在显著的爬升,水体的爬升带动营养盐上升,在水深200~600m处与其他水团扰动混合,容易形成渔场。 | 王冬 黄洪亮 张钟哲 伍玉梅 李灵智 陈帅 屈泰春 | 2016 | 海洋科学进展2016，34，2： | 2 |
您所在的机构暂未开通此部分的功能，请联系管理员