Study on Distribution Characteristics of Evaporation Duct for Electromagnetic Wave Propagation

Haichuan Tang, Yu Zhang, Hua Wang, Xiang-jun Yu
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引用次数: 1

Abstract

Evaporation duct widely exists in the ocean, which has an important impact on shipborne electronic equipment. The application of an evaporation duct requires mastering the distribution characteristics of an evaporation duct. Based on the ERA-Interim surface data released by ECMWF from 2011 to 2015, the P-J evaporation duct model is used to analyze the distribution of global evaporation ducts. It is concluded that the average height of the evaporation duct is zonally distributed, which can be divided into seven zones, from low to high latitudes, the lower-value zone of the tropical convergence zone, the high- value zone of the north trade wind zone, the high-value zone of the south trade wind zone, the transition zone of the northern hemisphere, the transition zone of the southern hemisphere, the low-value zone in northern hemisphere and southern hemisphere; the height of the evaporation duct is relatively low on the cold current areas, and relatively high on the warm current areas; the evaporation duct has not only geographical variation but also seasonal variation. The seasonal variation in the location of the lower value zone of the tropical convergence zone are roughly the same as that of the equatorial convergence zone. It is located at the southernmost point in February and the northernmost point in August. The location of high-value areas of trade wind has the same seasonal variation. The height of the evaporation duct in high-value areas of trade wind is higher in the season with relatively strong trade wind and low relative humidity, and lower in the season with relatively weak trade wind and high relative humidity.
电磁波传播蒸发管道分布特性研究
蒸发管在海洋中广泛存在,对船载电子设备有重要影响。蒸发风管的应用需要掌握蒸发风管的分布特性。基于2011 - 2015年ECMWF发布的ERA-Interim地表数据,采用P-J蒸发风道模型对全球蒸发风道分布进行了分析。结果表明:蒸发风道平均高度呈纬向分布,从低纬度到高纬度可划分为热带辐合带低值区、北信风带高值区、南信风带高值区、北半球过渡区、南半球过渡区、北半球和南半球低值区;冷流区蒸发风管高度相对较低,暖流区蒸发风管高度相对较高;蒸发管道不仅具有地理上的差异,而且具有季节上的差异。热带辐合带低值带位置的季节变化与赤道辐合带大致相同。它位于二月的最南端和八月的最北端。信风高值区位置具有相同的季节变化。信风高值区蒸发风管高度在信风较强、相对湿度较低的季节较高,在信风较弱、相对湿度较高的季节较低。
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