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Fronts and Mesoscale Variability in the Southern Indian Ocean as Inferred from the TOPEX/POSEIDON and ERS-2 Altimetry Data

机译:根据TOPEX / POSEIDON和ERS-2测高数据推论的南印度洋的锋面和中尺度变率

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摘要

Charts of sea level anomalies (SLA) based on the combined altimetry data from the TOPEX/POSEIDON and ERS-2 satellites,as well as the corresponding charts of the sea surface dynamic heights (constructed by the superposition of SLA distributions over the climatic dynamic topography) and the temperature gradients at the ocean surface on the basis of the satellite Multi-Channel Sea Surface Temperature temperature gradients at the ocean surface on the basis of the satellite Multi-Channel Sea Surface Temperature (MCSST) data,were used to study the mesoscale variability related to the fronts in the Southern Indian Ocean (30 deg -60 deg S,20 deg-150 deg E).An analysis of these three ty0pes of satellite information for the central weeks of each month during the period from 1997 to 1999 allowed us to distinguish zones of enhanced meandering ?(eddy for-mation)within the basin under study,as well as the contributions of individual fronts and their interaction to the regional mesoscale variability.The problems of the correlation between the intensity of mesoscale variability and peculiarities of the local bottom topography and seasonal/interannual variability of mesoscale dynamics are addressed.
机译:基于来自TOPEX / POSEIDON和ERS-2卫星的组合测高数据的海平面异常(SLA)图以及相应的海面动态高度图(由SLA分布在气候动态地形上的叠加构成) )和基于卫星多通道海面温度的海面温度梯度,并基于卫星多通道海面温度(MCSST)数据的海面温度梯度,用于研究中尺度与南印度洋锋面(30度-60度南极,20度​​-150度东极)有关的变异性。对1997年至1999年期间每个月的中央周的这三种卫星信息进行分析我们要区分研究盆地内弯曲曲率增强的区域(涡形),以及各个锋面的贡献及其对区域中尺度变化的相互作用。解决了中尺度变化的强度和局部底部地形的特殊性与中尺度动力学的季节/年际变化之间的相关性问题。

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