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Modelling surface currents in the Eastern Levantine Mediterranean using surface drifters and satellite altimetry

机译:使用表面漂移器和卫星测高仪对地中海东部黎凡特的地表水流进行建模

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We present a new and fast method that blends altimetric and drifter positions data in order to predict the surface velocity in the Eastern Levantine Mediterranean. The method relies on a variational assimilation approach where a velocity correction is continuously obtained by matching observed drifter positions with those predicted by a simple advection model. The background velocity used in the advection of the drifters is the aggregate of a geostrophic and a wind-driven component and the velocity correction is constrained to be divergence free. The algorithm employs a sliding time window that assimilates at once and inside each frame, an entire trajectory of drifters. We show that with few drifters, our method improves the estimation of velocity in two typical situations: an eddy between the Lebanese coast and Cyprus, and velocities along the Lebanese coast. (C) 2016 Elsevier Ltd. All rights reserved.
机译:我们提出了一种新的,快速的方法,它将高程和漂流者的位置数据融合在一起,以便预测东黎凡特地中海的地表速度。该方法依赖于变分同化方法,在该方法中,通过将观测到的漂流位置与简单对流模型预测的位置相匹配,可以连续获得速度校正。漂移平流中使用的背景速度是地转和风驱动分量的总和,速度校正被约束为无散度。该算法采用一个滑动时间窗口,该时间窗口在每个帧的内部和同时漂移,整个漂移轨迹。我们表明,在很少的漂流情况下,我们的方法可以改善两种典型情况下的速度估算:黎巴嫩海岸和塞浦路斯之间的涡流以及黎巴嫩海岸的速度。 (C)2016 Elsevier Ltd.保留所有权利。

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