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- W3142590900 abstract "当自台湾东面的菲律宾海流向日本的暖流的时间空间的可变性被 mesoscale 旋涡高度影响，代表它的季节的可变性特征要求足够地长期的观察减少无常。从 1987 ～ 2010 从水道学的观察估计的因地球自转而引起的速度数据和在在中央华东海的 PN 节的从 1993 ～ 2008 的舷侧 ADCP 速度数据被收集客观地看季节的可变性。从观察的两种类型，自台湾东面的菲律宾海流向日本的暖流水流的季节的气候学平均数在三个区域展出重要差别，这被发现，它在自台湾东面的菲律宾海流向日本的暖流当前的核心和它的二胁腹位于浅层不到 300 m ，与在在秋天的核心的最弱的东北水流，在春天的正确胁腹上的最强壮的相反的水流，和在秋天的左胁腹上的最强壮的东北水流分别地。自台湾东面的菲律宾海流向日本的暖流水流的季节的变化也展出重要差别在上近海自台湾东面的菲律宾海流向日本的暖流的方面，与在春天和夏天的更大的变化当时在秋天和冬季的更小的变化。为到 PN 节的当前的平行，到 intraseasonal 可变性部件的季节的可变性部件的比率为对 PN 节垂直的水流是比那相对小的。进一步的分析显示在 PN 节的季节的可变性紧被连接到在上游、下游的当前的可变性。" @default.
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- W3142590900 date "2015-01-01" @default.
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- W3142590900 title "Seasonal variability of the Kuroshio Current at the PN Section in the East China Sea based on in-situ observation from 1987 to 2010" @default.
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