1) Kuroshio branches east of Taiwan Island
台湾岛以东黑潮分支
2) Kuroshio east of Taiwan Island
台湾岛以东黑潮
1.
Based on the wind and hydrographic data obtained from the cruise of the China - Japan Joint Investigation on Subtropical Circulation System in December 1997, the Kuroshio east of Taiwan Island and the currents southeast of the Ryukyu-gunto are computed by three-dimensional nonlinear diagnostic, semidiagnostic and prognostic models in the σ coordinate.
基于1997年12月“中日副热带环流合作调查”航次获得的水文和气象资料,采用海流三维非线性的诊断、半诊断及预报模式计算了台湾岛以东黑潮及琉球群岛东南海域海流。
4) Kuroshio east of Taiwan Island and in the East China Sea during winter
冬季台湾岛以东及东海黑潮
5) Kuroshio east of Taiwan Island and in East China Sea during summer
夏季台湾岛以东及东海黑潮
6) Kuroshio transport
台湾以东黑潮流量
1.
Using the NCAR/NCEP reanalysis (1958—1999), COADS monthly data(1945—1993) and Kuroshio transport observation from various sources covering 1980—1997, we studied mainly the relationship between Kuroshio transport and ocean-atmosphere interaction in the area northeast of Taiwan in Northwest Pacific (NWP) during winter.
通过对历史资料进行奇异值分解、合成分析及相关分析,揭示了对应冬季台湾以东黑潮流量增强(减弱)时,西北太平洋海区异常失热(得热),北太平洋(北纬20°N以北)上空500hPa位势高度负异常(正异常);进一步证实了冬季西北太平洋海洋-大气相互作用是一个正反馈过程;发现了冬季台湾以东黑潮的暖平流作用可能是维持该正反馈过程进行的一个必要条件;通过超前和滞后相关及合成分析,提出从10月开始,台湾以东黑潮流量异常形成的暖平流作用会对冬季西北太平洋海区海洋-大气相互作用有贡献。
补充资料:琉球岛位于中国台湾省
琉球岛位于中国台湾省
漂 琉球岛位于中国台湾省马志华供稿
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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