中国近海岸基GNSS-R探测蒸发波导的空间范围研究

Research on Spatial Range of GNSS-R Detection of Evaporation Duct in the Coastal Waters of China

  • 摘要: 蒸发波导由于其折射效应对雷达、通信具有显著影响。GNSS-R(Global Navigation SatelliteSystems Reflectometry)全天候、被动接收的特点使其具有探测蒸发波导的应用潜力,然而岸基GNSS-R探测的空间范围与蒸发波导高度密切相关,在中国近海复杂的蒸发波导环境下是否具备实用价值仍有待研究。因此,基于沿海气象观测站实测数据以及欧洲中期天气预报中心(ECMWF)发布的海水表面温度数据,采用蒸发波导预测模型与GNSS-R蒸发波导探测范围模型,系统分析了GNSS-R探测蒸发波导的空间范围的时空分布特征。结果表明,基于中国沿海气象数据得到的GNSS-R探测蒸发波导的空间范围在UTC时间5点至7点达到峰值,至夜间逐渐降低并趋于稳定;季节变化方面,夏秋季平均探测范围最大,冬季最小,在蒸发波导的高发期和平静期,GNSS-R探测蒸发波导的空间范围的平均值分别为145km和103km;此外地域地形差异对探测范围也有影响,辽东半岛以及海南岛西侧探测范围平均值均大于东侧,而台湾海峡作为蒸发波导的高发区域,其GNSS-R探测蒸发波导的空间范围明显大于周边海域。这一研究结果将扩展气象数据的应用领域,提高相关区域雷达探测效能,并且为通信提供干扰预警信息。

     

    Abstract: Objectives: The evaporation duct has a significant impact on shore based radar, shipborne radar, and 5G communication due to its refractive effect. GNSS-R has the application potential of detecting evaporation duct due to the characteristics of all-weather, passive reception and high spatial and temporal resolution. However, spatial range of GNSSR detection of evaporation duct is closely related to the evaporation duct height, and whether it has practical value in the complex evaporation duct environment near the coast of China still needs to be studied. Methods: Thus, meteorological data measured from coastal meteorological observation stations and sea surface temperature released by ECMWF were used to obtain the spatiotemporal distribution pattern of the spatial range of GNSS-R detection of evaporation duct, which the evaporation duct model and GNSS-R evaporation duct detection range model are adopted. Results: The results indicate that the spatial range of GNSS-R detection of evaporation duct based on Chinese coastal meteorological data first increases and then decreases during the day, reaches maximum from 5:00 to 7:00 UTC, and gradually decreases and stabilizes at night. In terms of seasonal changes, the highest is reached in summer and autumn, and the lowest is in winter. The detection range of the Bohai Sea and Yellow Sea are greatly affected by seasons, while the detection range of the East China Sea and South China Sea is large and remains relatively stable throughout the year, especially in the South China Sea, it can maintain a detection range of about 130km throughout the year. Further analysis found that during the high incidence period and the quiet period of the evaporation duct, the average spatial range of GNSS-R detection of the evaporation duct is 145km and 103km, respectively. In addition, regional differences have an influence on the detection range, for example, the average spatial range of GNSS-R detection of evaporation duct on the western side of Liaodong Peninsula and Hainan Island is greater than that on the eastern side, and the Taiwan Strait, as a high incidence area for evaporation ducts, has a larger spatial range for GNSS-R detection of evaporation ducts than the surrounding waters. Conclusions: The analysis results can expand the application areas of meteorological data, improve radar detection efficiency in relevant areas, and provide the warning information for communication.

     

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