极地研究(英文版)2008,Vol.19Issue(2):123-134,12.
Toward development of the 4Dvar data assimilation system in the Bering Sea: reconstruction of the mean dynamic ocean topography
Toward development of the 4Dvar data assimilation system in the Bering Sea: reconstruction of the mean dynamic ocean topography
摘要
Abstract
The Bering Sea circulation is derived as a variational inverse of hydrographic profiles( temperature and salinity) , atmospheric climatologies and historical observation of ocean curents. The important result of this study is estimate of the mean climatological sea surface height (SSH) that can be used as a reference for satellite altimetry sea level anomaly data in the Bering Sea region. Numerical experiments reveal that, when combined with satellite altimetry, the obtained reference SSH effectively constrains a realistic reconstruction of the Amukta Pass circulation.关键词
Bering Sea/mean dynamic ocean topography/4Dvar data assimilation systemKey words
Bering Sea/mean dynamic ocean topography/4Dvar data assimilation system引用本文复制引用
Gleb Panteleev,Dmitri Nechaev,Vladimir Luchin,Phyllis Stabeno,Nikolai Maximenko,Motoyoshi Ikeda..Toward development of the 4Dvar data assimilation system in the Bering Sea: reconstruction of the mean dynamic ocean topography[J].极地研究(英文版),2008,19(2):123-134,12.基金项目
This study was supported by North Pacific Research Board (NPRB),project No828,contribution No204,and by JAMSTEC,Japan,through the sponsorship of IARC. The study was also supported by the NSF Award 0629311 and RFFI Grant 06-05-96065.Nikolai Maximenko was partly supported by NASA through mem-bership in its Ocean Surface topography Science team. (NPRB)