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地球科学进展  2015, Vol. 30 Issue (5): 579-588    DOI: 10.11867/j.issn.1001-8166.2015.05.0579
综述与评述     
全球海潮模型研究进展
张胜凯1, 雷锦韬1, *, 李斐1, 2
1.中国南极测绘研究中心,武汉大学, 湖北 武汉 430079; 2.测绘遥感信息工程国家重点实验室,武汉大学, 湖北 武汉 430079
Advances in Global Ocean Tide Models
Zhang Shengkai1, Lei Jintao1, Li Fei1, 2
1. Chinese Antarctic Center of Surveying and Mapping, Wuhan University, Hubei 430079, China; 2. State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing, Wuhan University, Wuhan 430079, China
 全文: PDF(4460 KB)  
摘要:

阐述潮汐分析方法和建模方法,归纳总结了FES,CSR,GOT,NAO,TPXO,EOT,DTU,HAMTIDE及OSU系列全球海潮模型的建立机构、使用数据及构建方法等。对比分析2010年后出现的几种新的海潮模型(FES2012,EOT11a,DTU10和HAMTIDE11a)在南大洋的M2振幅,发现模型间差异主要集中在浅水及极地地区,其中极地地区高精度卫星测高数据的缺少及海冰的季节性变化,是导致建模精度较差的主要原因。最后对海潮模型的发展方向提出一些建议。

关键词: 卫星测高潮汐分析南极验潮站海潮模型    
Abstract:

The theories of tidal analysis and methods of ocean tide modeling are presented at first,and a series of global ocean tide models (FES,CSR,GOT,NAO,TPXO,EOT,DTU,HAMTIDE and OSU) are summarized, including their affiliations, data, and methods of modeling. The amplitude differences of M2 constituent of four new models (FES2012,EOT11a,DTU10,HAMTIDE11a) which released after 2010 are provided to show that shallow-water and polar sea are the main different regions. The main reasons leading to a poor accuracy in polar sea tidal modeling are the lack of highly accurate altimetry data and the presence of sea ices. Some suggestions are proposed for the future study of ocean tide modeling.

Key words: Ocean Tide Model    Tide gauge    Satellite altimetry    Antarctica.    Tidal analysis
出版日期: 2015-05-06
:  P731.23  
基金资助:

国家重大科学研究计划项目“近百年极地冰层和全球及典型区域海平面变化机理精密定量研究”(编号:2012CB957701); 国家自然科学基金项目“利用CryoSat-2和GPS进行东南极冰盖/冰架变化研究”(编号:41176173)资助

通讯作者: 雷锦韬(1988-),男,广西桂林人,硕士研究生,主要从事大地测量学在极地的应用研究.      E-mail: jintao.lei@whu.edu.cn
作者简介: 张胜凯(1977-),男,山东东明人,副教授,主要从事极地大地测量学与冰川动力学研究.E-mail:zskai@whu.edu.cn
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引用本文:

张胜凯, 雷锦韬, 李斐. 全球海潮模型研究进展[J]. 地球科学进展, 2015, 30(5): 579-588.

Zhang Shengkai, Lei Jintao, Li Fei. Advances in Global Ocean Tide Models. Advances in Earth Science, 2015, 30(5): 579-588.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2015.05.0579        http://www.adearth.ac.cn/CN/Y2015/V30/I5/579

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