O437∥TN918 98042405光学双稳系统混沌驱动保密通讯原理研究=Study ofmachanism of secure communication with driv-en chaos masking in optical bistable system[刊,中]/刘金刚,周立伟(北京理工大学工程光学系.北京(100081)),沈柯(...O437∥TN918 98042405光学双稳系统混沌驱动保密通讯原理研究=Study ofmachanism of secure communication with driv-en chaos masking in optical bistable system[刊,中]/刘金刚,周立伟(北京理工大学工程光学系.北京(100081)),沈柯(长春光机学院理学分院.吉林。展开更多
O437 99031626茶溶液中饱和吸收产生热致非线性效应的研究=Study of optical nonlinearities induced by thermaleffect from saturable absorption in tea liquid[刊,中]/贾振红(新疆大学电子信息科学系.新疆,乌鲁木齐(830046)),吴树荣...O437 99031626茶溶液中饱和吸收产生热致非线性效应的研究=Study of optical nonlinearities induced by thermaleffect from saturable absorption in tea liquid[刊,中]/贾振红(新疆大学电子信息科学系.新疆,乌鲁木齐(830046)),吴树荣(新疆大学物理系.新疆,乌鲁木齐(830046)),李劬(上海交通大学应用物理系.上海(200030))//激光杂志.—1998,19(1).展开更多
Absolute geostrophic currents in the North Pacific Ocean were calculated using P-vector method from newly gridded Argo profiling float data collected during 2004-2009. The meridional volume transport of geostrophic cu...Absolute geostrophic currents in the North Pacific Ocean were calculated using P-vector method from newly gridded Argo profiling float data collected during 2004-2009. The meridional volume transport of geostrophic currents differed significantly from the classical Sverdrup balance, with differences of 10×106 -20×106 m3 /s in the interior tropical Northwest Pacific Ocean. Analyses showed that errors of wind stress estimation could not explain all of the differences. The largest differences were found in the areas immediately north and south of the bifurcation latitude of the North Equatorial Current west of the dateline, and in the recirculation area of the Kuroshio and its extension, where nonlinear eddy activities were robust. Comparison of the geostrophic meridional transport and the wind-driven Sverdrup meridional transport in a high-resolution OFES simulation showed that nonlinear effects of the ocean circulation were the most likely reason for the differences. It is therefore suggested that the linear, steady wind-driven dynamics of the Sverdrup theory cannot completely explain the meridional transport of the interior circulation of the tropical Northwest Pacific Ocean.展开更多
基金supported by China National Funds for Distinguished Young Scientists(51225504)National Natural Science of China(91123016)program for the Top Young Academic Leaders of Higher Learing Institutions of Shanxi
文摘O437∥TN918 98042405光学双稳系统混沌驱动保密通讯原理研究=Study ofmachanism of secure communication with driv-en chaos masking in optical bistable system[刊,中]/刘金刚,周立伟(北京理工大学工程光学系.北京(100081)),沈柯(长春光机学院理学分院.吉林。
文摘O437 99031626茶溶液中饱和吸收产生热致非线性效应的研究=Study of optical nonlinearities induced by thermaleffect from saturable absorption in tea liquid[刊,中]/贾振红(新疆大学电子信息科学系.新疆,乌鲁木齐(830046)),吴树荣(新疆大学物理系.新疆,乌鲁木齐(830046)),李劬(上海交通大学应用物理系.上海(200030))//激光杂志.—1998,19(1).
基金Supported by the National Basic Research Program of China(973 Program)(No.2012CB956000)the National Natural Science Foundation of China(Nos.40888001,41176019)supported by KLOCAW1208
文摘Absolute geostrophic currents in the North Pacific Ocean were calculated using P-vector method from newly gridded Argo profiling float data collected during 2004-2009. The meridional volume transport of geostrophic currents differed significantly from the classical Sverdrup balance, with differences of 10×106 -20×106 m3 /s in the interior tropical Northwest Pacific Ocean. Analyses showed that errors of wind stress estimation could not explain all of the differences. The largest differences were found in the areas immediately north and south of the bifurcation latitude of the North Equatorial Current west of the dateline, and in the recirculation area of the Kuroshio and its extension, where nonlinear eddy activities were robust. Comparison of the geostrophic meridional transport and the wind-driven Sverdrup meridional transport in a high-resolution OFES simulation showed that nonlinear effects of the ocean circulation were the most likely reason for the differences. It is therefore suggested that the linear, steady wind-driven dynamics of the Sverdrup theory cannot completely explain the meridional transport of the interior circulation of the tropical Northwest Pacific Ocean.
