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基于再分析数据的南大洋区域Ekman流时空分布规律研究
引用本文:林辉义,高艳秋,张继才.基于再分析数据的南大洋区域Ekman流时空分布规律研究[J].海洋与湖沼,2021,52(4):860-873.
作者姓名:林辉义  高艳秋  张继才
作者单位:浙江大学海洋学院物理海洋与遥感研究所 舟山 316021;自然资源部第二海洋研究所卫星海洋环境动力学国家重点实验室 杭州 310012
基金项目:国家重点研发计划“全球变化及应对”重点专项,2017YFA0604100号;国家重点研发计划“海洋环境安全保障”重点专项,2017YFC1404000号;国家自然科学基金,41876086号;国家自然科学基金,41706006号。
摘    要:南大洋Ekman输运是全球大气-海洋耦合气候系统的重要组成部分,对该区域Ekman动力过程的研究极为重要.首先基于实测数据和文献资料,对GEKCO2 (Geostrophic and Ekman Current Observatory 2)产品提供的Ekman流数据进行了评估,验证了数据的有效性;并结合CCMP(cro...

关 键 词:南大洋  Ekman流  时空变化  经验正交函数分析法  海表洋流产品GEKCO2
收稿时间:2021/1/11 0:00:00
修稿时间:2021/3/4 0:00:00

THE SPATIAL AND TEMPORAL DISTRIBUTION OF EKMAN CURRENT IN THE SOUTHERN OCEAN BASED ON REANALYSIS DATA
LIN Hui-Yi,GAO Yan-Qiu,ZHANG Ji-Cai.THE SPATIAL AND TEMPORAL DISTRIBUTION OF EKMAN CURRENT IN THE SOUTHERN OCEAN BASED ON REANALYSIS DATA[J].Oceanologia Et Limnologia Sinica,2021,52(4):860-873.
Authors:LIN Hui-Yi  GAO Yan-Qiu  ZHANG Ji-Cai
Institution:Institute of physical oceanography and remote sensing, Ocean College, Zhejiang University, Zhoushan 316021, China;State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resource, Hangzhou 310012, China
Abstract:Ekman transport in the Southern Ocean is an important part of the global atmosphere ocean coupled climate system. It is very important to study the Ekman dynamic process in this region. The Ekman current data provided by GEKCO2 product was evaluated and its validity verified. In addition, combined with sea surface wind products (CCMP and ERA5), EOF analysis and other methods were used to analyze the spatial and temporal variation of Ekman current in the Southern Ocean from 2010 to 2018. Results show that first, the speed of Ekman current ranged 9-11 cm/s with a strong inter-monthly oscillation (the strongest in July and the weakest in December). Secondly, the speed of Ekman current varied greatly with time north of 40°S in the Southern Ocean. Thirdly, The EOF analysis of the speed of Ekman current indicates that the first mode had a strong correlation with the wind field, in which the speed increased or decreased at the same time on the whole. The second mode had a strong correlation with the middle and high latitude atmospheric circulation in the southern hemisphere, in which the speed from north to south was reversed with 50°S as the boundary. Fourthly, the left deviation angle of Ekman current was distributed in the range of 60° to 75° with the maximum probability density at 67.5°. Through the analysis of complex correlation, it was found that the average deviation angle in the area of 30-35°S varied monthly. This study provides a reference for further understanding of the Ekman process in the Southern Ocean.
Keywords:the Southern Ocean  Ekman current  spatial and temporal variation  empirical orthogonal function (EOF) analysis  ocean current product GEKCO2 (Geostrophic and Ekman Current Observatory 2)
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