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首页> 外文期刊>Indian Journal of Marine Sciences >Use of ERS-1 scatterometer and Topex altimeter data in a nonlinear reduced gravity model of the northwestern Indian Ocean
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Use of ERS-1 scatterometer and Topex altimeter data in a nonlinear reduced gravity model of the northwestern Indian Ocean

机译:在西北印度洋的非线性降重力模型中使用ERS-1散射仪和Topex高度计数据

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This paper describes the use of ERS-1 scatterometer winds and sea level from Topex altimeter in the simulations of oceanic circulation during the monsoon season by a nonlinear reduced gravity model of the northwestern Indian Ocean. Results have been presented for June and July 1993. In the first case, monthly means of ERS-1 scatterometer winds have been used for model forcing while in the second case the analysed winds provided by Florida State University (FSU) have been used. For both the cases, sea level provided by Topex altimeter has been used to initialise the model. The model generated sea level variability has been compared with altimeter sea level variability for the months of June and July . The model results with scatterometer wind forcing are in better agreement with altimeter data of the same month and produce additional eddy near Socotra island which is not observed in the case of FSU wind forcing. Thus satellite data have significant use in the simulation of oceanic circulation.
机译:本文通过西北印度洋的非线性降重力模型,描述了Topex高度计中ERS-1散射仪的风速和海平面在季风季节海洋循环模拟中的使用。给出了1993年6月和1993年7月的结果。在第一种情况下,使用ERS-1散射仪风的月平均值进行模型强迫,而在第二种情况下,使用了佛罗里达州立大学(FSU)提供的分析风。对于这两种情况,都使用了Topex高度计提供的海平面来初始化模型。该模型产生的海平面变异性已与6月和7月的高度计海平面变异性进行了比较。散射计测风的模型结果与当月的高度计数据更加吻合,并且在索科特拉岛附近产生了额外的涡流,而在FSU测风的情况下则没有观察到。因此,卫星数据在模拟海洋环流中具有重要用途。

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