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A Study on the ENSO Effects on the Sea Level of the Java Sea Using the Time Lag Analysis and an Oceanic General Circulation Model

机译:时滞分析和海洋总环流模型研究ENSO对爪哇海平面的影响

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The El Ni?o Southern Oscillation (ENSO) effects on the sea level of the Java Sea are studied using the time lag analysis and the Hybrid Coordinate Ocean Model (HYCOM). The time lag analysis results show that the time lags among wind, Southern Oscillation Index (SOI) and sea level changes are 0 to 2 month lag. The HYCOM-estimated sea levels are validated using tide gauge sea levels. Due to the shallowness of the Java Sea, the wind-induced mixed layer is easily reaches to the bottom. The HYCOM-estimated volume transport is compared with European Remote Sensing (ERS) satellite wind vectors. The HYCOM results show that the ENSO effects on the sea level greater than the wind effect.
机译:使用时滞分析和混合坐标海洋模型(HYCOM)研究了厄尔尼诺南方涛动(ENSO)对爪哇海海平面的影响。时滞分析结果表明,风,南方涛动指数(SOI)和海平面变化之间的时滞为0至2个月时滞。 HYCOM估计的海平面已使用潮汐仪海平面进行了验证。由于爪哇海的浅浅,风致混合层很容易到达底部。将HYCOM估算的体积传输与欧洲遥感(ERS)卫星风向矢量进行比较。 HYCOM结果表明,ENSO对海平面的影响大于风的影响。

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