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Sensitivity of the northwestern Mediterranean Sea coastal and thermohaline circulations simulated by the 1/12°-resolution ocean model NEMO-MED12 to the spatial and temporal resolution of atmospheric forcing

机译:1/12°分辨率海洋模型NEMO-MED12模拟的西北地中海沿岸和热盐环流对大气强迫的时空分辨率的敏感性

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The northwestern Mediterranean (NWM) Sea is prone to intense weather events, associated with high winds, that are characterized by strong shallow jets and a high spatial and temporal variability. The ocean response in this area is very sensitive to the atmospheric conditions, particularly in the Gulf of Lions coastal zone.The ocean response to strong winds is here investigated using the NEMO-MED12 eddy-resolving model, driven by four atmospheric forcings differing in spatial resolution (20 km, 6.7 km) and temporal resolution (daily or 3 h) and produced with the non-hydrostratic mesoscale WRF model.The noticeable effects of the higher-frequency forcing are (i) to reduce the shelf dense-water formation and the deep offshore convection in winter due to the explicit simulation of the diurnal cycle that warms and stratifies the ocean upper layers and (ii) to increase the vertical velocity in the upwelling cells. The higher spatial resolution allows, in particular, the production of stronger winds and the accurate repro-duction of the near-surface sub-mesoscale eddies in the coastal areas, in agreement with observations.
机译:地中海西北海(NWM)容易发生强烈的天气事件,伴随着强风,其特征是强烈的浅水喷射和高的时空变异性。该区域的海洋响应对大气条件非常敏感,特别是在狮子湾沿岸地区。在此,我们使用NEMO-MED12涡旋解析模型研究了强风对海洋的响应,该模型由四个在空间上不同的大气强迫驱动分辨率(20 km,6.7 km)和时间分辨率(每天或3 h)并由非水文中尺度WRF模型产生。高频强迫的显着效果是(i)减少了架子上密集水的形成和冬季深层对流活动是由于对昼夜周期进行了明确模拟,使海洋上层变暖和分层,并且(ii)增加了上升流单元的垂直速度。更高的空间分辨率尤其允许在沿海地区产生更强的风,并准确再现沿海地区的近地表亚中尺度涡流。

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