汤博^1,2,3,4, 侯一筠^1,2,3,4,5, 殷玉齐^1,2,4,5, 胡珀^1,2,4,5
1.中国科学院海洋研究所, 山东 青岛 266071;2.中国科学院海洋环流与波动重点实验室, 山东 青岛 266071;3.中国科学院大学, 北京 100049;4.中国科学院海洋大科学研究中心, 山东 青岛 266071;5.青岛海洋科学与技术试点国家实验室海洋动力过程与气候功能实验室, 山东 青岛 266237

摘要:
利用历史观测得到的温度剖面数据，通过严格筛选和插值，建立了南海北部的气候态垂向温度剖面。随后，利用回归统计分析的方法构建了海面温度异常（SSTA）、海面高度异常（SSHA）联合扩展温度剖面的经验回归模型，并采用卫星遥感得到的SST和SSH数据扩展了南海北部的三维海洋温度场，其时间分辨率为天，空间分辨率为0.25°×0.25°。通过与观测数据的对比研究，扩展得到的温度场可以较为准确地反映南海北部温度剖面的结构特征，并且能有效地体现出一些中尺度变化过程。结果表明，本研究反演得到的三维温度扩展场是较为可靠的，它可以作为海洋数值模型的初始场，实现现场观测数据和卫星遥感数据的互补，有助于更好地分析南海北部温度场的三维结构及变化特征。
关键词:南海北部卫星遥感海面温度(SST)和海面高度(SSH)反演三维温度场
DOI：10.11759/hykx20190312002
分类号:P722.7
基金项目:国家重点研究发展项目（2016YFC1400100）；国家自然科学基金（41630967）；“全球变化与海气相互作用”专项项目（GASI-IPOVAI-01-06）；国家自然科学基金-山东省联合资助海洋科学研究中心项目（U1606402）；国家自然科学基金创新研究群体项目（41421005）

Inversion of the three-dimensional temperature field in the northern part of the South China Sea based on the remote satellite sea surface temperature and height
TANG Bo^1,2,3,4, HOU Yi-jun^1,2,3,4,5, YIN Yu-qi^1,2,4,5, HU Po^1,2,4,5
1.Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;2.Key Laboratory of Ocean Circulation and Wave, Chinese Academy of Sciences, Qingdao 266071, China;3.University of Chinese Academy of Sciences, Beijing 100049, China;4.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;5.Laboratory for Ocean and Climate Dynamics, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266237, China
Abstract:
On the basis of historically observed temperature profile data, a static climate temperature field was established through strict screening and interpolation. Then, regression analysis was used to build an empirical regression model to invert temperature profiles based on the sea surface temperature (SST) and sea surface height (SSH) anomalies. Finally, a three-dimensional temperature field was expanded in the northern part of the South China Sea using the remote satellite SST and SSH, whose temporal resolution is daily and spatial resolution is 0.25°×0.25°. Compared with the observational data, the expanded temperature field can accurately reflect the structure of the temperature profiles and can well describe some mesoscale variabilities in the northern part of the South China Sea. Results showed that the expanded temperature field is reliable and can be used as the initial field of the numerical model to determine the complementarity between observed and satellite data. Thus, a more in-depth analysis of the three-dimensional structure and variation characteristics of the temperature profiles in the northern part of the South China Sea can be conducted.
Key words:northern part of the South China Seasatellite sea surface temperature and heightinversion of the three-dimensional temperature field





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