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Interannual and Decadal Variation of Sea level in the East China Sea

机译:东海海平面的年际和年代际变化

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Sea level variation and its dynamic and thermal processes wereinvestigated with the TOPEX/Poseidon (T/P) altimeter data,reconstructed sea level data and tide gauge records on the interannualand decadal scale in the East China Sea (ECS). Stochastic dynamicmethod was used to analyze the characteristics of sea level variation.During 1993 to 2010, the sea level rising rate of the whole ECS was2.5mm/a. The interannual and decadal sea level variations wereremarkable and, focused on 2~4 and 8~10 years. The interannual sealevel variation was influenced by ENSO and the amplitudes mappednon-uniform spatially. The interannual amplitude was less than 5 cm,which steric effects contributed 65%.The correlation between steric sealevel and sea level can reach to 0.93. We found that ocean currents andzonal wind stress exhibited as the main oceanic dynamic factors toinfluence the interannual sea level variation in the ECS, as well as thevertical structure and its changes of temperature and salinity. Bycomparing sea level anomaly with wind stress in the ECS on theinterannual scale, their correlation coefficient was up to -0.65, when thesea level lagged zonal wind stress 3 months. On the decadal scale, windstress and steric effects acted as the important physical processescontributing to the sea level variation.
机译:利用TOPEX / Poseidon(T / P)高度计数据,重建的海平面数据和东海年际和年代际尺度的潮汐记录记录,研究了海平面变化及其动态和热过程。运用随机动态方法对海平面变化特征进行分析。1993年至2010年,整个ECS海平面上升速度为2.5mm / a。年际和年代际海平面变化明显,主要集中在2〜4年和8〜10年。年际海平面变化受到ENSO的影响,其幅度映射在空间上不均匀。年际振幅小于5 cm,空间效应贡献65%。空间海平面与海平面的相关性可达到0.93。我们发现洋流和纬向风应力是影响ECS年际海平面变化以及温度和盐度垂直结构及其变化的主要海洋动力因素。在年际尺度上,通过比较海平面异常与风应力,当海平面滞后纬向风应力3个月时,它们的相关系数高达-0.65。在十年尺度上,风应力和空间效应是导致海平面变化的重要物理过程。

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