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Seasonal and interannual variations of the Leeuwin Current off Western Australia from TOPEX/Poseidon satellite altimetry

机译:TOPEX / Poseidon卫星测高仪在西澳大利亚州产生的Leeuwin流的季节和年际变化

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摘要

The Leeuwin Current (LC) is an eastern boundary current flowing strongly southwards along the Western Australian coastline. The current varies seasonally, with weaker southwards flow occurring during the austral summer (November to March), when southerly winds are strongest. Nearly 9.5 years of TOPEX/Poseidon-derived sea-surface heights, in conjunction with the AUSGeoid98 gravimetric geoid model, have been used to investigate the temporal characteristics of the LC over the area bounded by 20 to 45 degrees S and 108 to 130 degrees E. The ocean dynamic height associated with the LC is used to compute the geostrophic parameters of volume transport, axis velocity, height jump, width, and axis locations of the current: These parameter estimates are then used to analyse the seasonal and interannual variability of the LC, as well as effects related to the El Nino Southern Oscillation (ENSO). Our results show that the LC is highly variable in terms of seasonal volume transport and is closely linked to ENSO events at interannual time-scales. Seasonally, when assuming an averaged isobath of 80 m, the LC has maximum volume transport of up to -7.2 Sv (10(6) m(3) s(-1), a negative sign means southwards transport) in April - June and -8.4 Sv in May - August in regions west and south of Western Australia, respectively. Inter-annually, the LC has higher volume transports than the average transport during 1993 - 2003 in most La Nina years, and the opposite in most El Nino years, which is linked to inter-basin exchange between the Pacific and Indian Oceans.
机译:Leeuwin洋流(LC)是沿着西澳大利亚州海岸线强烈向南流动的东部边界流。潮流随季节变化,在南风最大的夏季(11月至3月),南风减弱。 TOPEX /波塞冬派生的海面高度将近9.5年,结合AUSGeoid98重力大地水准面模型,已用于研究以20到45度S和108到130度E为界的LC的时间特征。与LC相关的海洋动态高度用于计算洋流的地转参数,洋流的速度,高度跳跃,宽度和洋流的轴位置:这些参数估计值然后用于分析洋流的季节和年际变化。 LC,以及与厄尔尼诺南方涛动有关的影响。我们的结果表明,LC在季节流量传输方面变化很大,并且在年际尺度上与ENSO事件密切相关。按季节,假设平均等距线为80 m,则LC在4月-6月的最大体积输运量为-7.2 Sv(10(6)m(3)s(-1),负号表示向南输运),并且五月至八月在西澳大利亚州西部和南部的-8.4 Sv。在1993年至2003年间,大多数拉尼娜年间,LC的年运输量均高于平均运输量,而在大多数El Nino年中则相反,这与太平洋和印度洋之间的流域间交换有关。

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