引用本文:
【打印本页】   【下载PDF全文】   View/Add Comment  Download reader   Close
←前一篇|后一篇→ 过刊浏览    高级检索
本文已被:浏览 1998次   下载 2020 本文二维码信息
码上扫一扫!
分享到: 微信 更多
太平洋海面粗糙度的计算及在ENSO期间的变化
过 杰1, 郭佩芳1, 周良明1
中国海洋大学环境学院
摘要:
利用TOPEX高度计风速资料,实现了对太平洋海面粗糙度 (z0)的计算。1997~1999年正是厄尔尼诺与拉尼娜事件发生时期,作者研究了1997~1999年z0在ENSO期间的变化后发现:(1)EI Nion发生期间赤道附近z0最大值在A,C,B 3个站点上移动;最小值在B,A 2个站点上移动。(2)Li Nina发生期间赤道附近z0最小值在A站点,最大值主要在B站点上。Li Nina发生期间,1999年15个站点z0均大于正常年份和EI Nion发生期间的15个站点z0。(3)ENSO期间,四季z0与正常年份相比都有显著改变。
关键词:  ENSO  厄尔尼诺  拉尼娜  海面粗糙度(z0)  海面风速  高度计
DOI:
分类号:
基金项目:
Calculation and ahanging of roughness of sea surface in Pacific Ocean in ENSO period
Abstract:
We calculated values of roughness in 15 points using wind speed by TOPEX satellite Altimeter. We studied the changes of roughness during 1997~1999 (ENSO period) and compared them with roughness in 1996. We find some characteristics as follows: The largest roughness nearby equator is moving from station A to station C to station B and the smallest roughness is moving from station B to station A during the EI Nion period. The smallest roughness is in station A and the largest roughness is in station B during LI Nina period. The roughness of 15 stations in 1999 is bigger than those in 1996, 1997, 1998. The roughness of 4 seasons has prominent change during ENSO period when compared with 1996.
Key words:  ENSO  EI Nion  La Nina  the roughness of the sea surface  sea surface wind speed  satellite altimeter
Copyright ©  Editorial Office for Marine Sciences Copyright©2008 All Rights Reserved
Supervised by: Chinese Academy of Sciences (CAS)   Sponsored by: Institute of Oceanology, CAS
Address: 7 Nanhai Road, Qingdao, China.  Postcode: 266071  Tel: 0532-82898755  E-mail: bjb@qdio.ac.cn
Technical support: Beijing E-Tiller Co.,Ltd.