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Seasonal variability in coastal fronts and its influence on sea surface wind in the Northern South China Sea

机译:南海北部沿海地区季节变化及其对海面风的影响

摘要

High-resolution reanalysis data of Sea Surface Temperature (SST) show pronounced seasonal variations in oceanic fronts in the coastal area of the Northern South China Sea (NSCS), which are accompanied by the seasonality of monsoons. The NSCS oceanic fronts cover a wider area of the coastal sea in winter than in summer as strong winter monsoons progress. Nonetheless, the average SST gradients of the frontal area in both seasons are comparable. The response of surface wind to SST perturbations attributed to oceanic fronts in the NSCS coastal area has also been investigated by the observation data of satellite borne scatterometers and the simulation data of the Weather Research and Forecasting (WRF) model. Both the satellite observations and the simulations of the WRF model show apparent positive linear SST-wind coupling for most months in 2008, indicating the local influence of coastal SST fronts on the sea surface wind in the NSCS. The SST-wind coupling coefficients in the NSCS coastal sea are larger than those observed at mid-latitude oceans but smaller than those observed near equatorial oceans. It is also found that the influence of topography on the sea surface wind could be more important than that of the SST front at the southern end of the Taiwan Strait in winter. The transition of the monsoon could also affect the SST-wind coupling in the NSCS. (C) 2013 Elsevier Ltd. All rights reserved.
机译:高分辨率的海面温度再分析数据显示,南海北部沿海地区(NSCS)海洋锋面出现明显的季节性变化,并伴有季风的季节变化。随着强烈的冬季风的发展,冬季与夏季相比,NSCS的海洋锋面覆盖的沿海海域面积更大。尽管如此,两个季节的额叶平均SST梯度是可比较的。还通过卫星散射仪的观测数据和天气研究与预报(WRF)模型的模拟数据,研究了表面风对NSCS沿海地区海面引起的SST扰动的响应。卫星观测结果和WRF模型的模拟结果都表明,在2008年的大部分月份中,SST-风的线性正相关性良好,表明沿海SST前沿对NSCS海面风的局部影响。 NSCS沿海海域的SST-风耦合系数大于中纬度海域的观测值,但小于赤道海域的观测值。还发现,冬季地形对海面风的影响可能比台湾海峡南端海表温度前的影响更为重要。季风的过渡也可能影响NSCS中的SST-风耦合。 (C)2013 Elsevier Ltd.保留所有权利。

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