针对目前带探头补偿的平面近远场变换中,探头H面方向图对远区副瓣引入较大误差的情况,结合国内传统的E面电场法和K.T.Selvan提出的边缘电流逼近法各自的优点,利用混合算法研究了一种新的探头方向图逼近公式,并将其应用于平面近场测试中...针对目前带探头补偿的平面近远场变换中,探头H面方向图对远区副瓣引入较大误差的情况,结合国内传统的E面电场法和K.T.Selvan提出的边缘电流逼近法各自的优点,利用混合算法研究了一种新的探头方向图逼近公式,并将其应用于平面近场测试中。通过在某大型微波暗室对一频段阵列天线进行实际测量,分别用E面电场法、边缘电流逼近法以及新的方法进行带探头补偿的近远场变换。最后,将各种方法与实际测试结果进行比较,求得其误差曲线,并在全域的角度分析各种方法的-50 d B超低副瓣精度。结果表明,此方法集合了前两种方法的优点,相比E面电场法,远区副瓣精度提高了8.2 d B,整个角域内副瓣精度提高了1.13 d B;相比边缘电流逼近法,近区副瓣精度提高了0.89d B,整个角域内副瓣精度提高了0.87d B。展开更多
Ten years （from 2005 to 2014） of satellite sea surface temperature （SST） data from the Advanced Very High Resolution Radiometer （AVHRR） are analyzed to reveal the monthly changes in surface cold patches （SCPs）...Ten years （from 2005 to 2014） of satellite sea surface temperature （SST） data from the Advanced Very High Resolution Radiometer （AVHRR） are analyzed to reveal the monthly changes in surface cold patches （SCPs） in the main areas of the Northern Yellow Sea （NYS）. The Canny edge detection algorithm is used to identify the edges of the patches. The monthly changes are de- scribed in terms of location, temperature and area. The inter-annual variations, including changes in the location and area of the SCPs from 2010 to 2014, are briefly discussed. The formation mechanisms of the SCPs in different periods are systematically analyzed using both in situ data and numerical simulation. The results show that from May to October, the location and area of the SCPs re- main stable, with a north-south orientation. The SCPs altogether cover about I° of longitude （124°E-125°E） in width and 2° of lati- tude （37.5°N-39.5°N） in length. In November, the SCP separates from the Jangsan Cape and forms a closed, isolated, and approxi- mately circular cold patch in the central NYS. From May to October, the upweUing that leads to the formation of the SCP is mainly triggered by the headland residual current, wind field, climbing movement of the current and secondary circulation at the tide front. In November, cyclonic circulation in the NYS is primarily responsible for generating the upwelling that leads to the formation of the closed and isolated SCE展开更多
文摘针对目前带探头补偿的平面近远场变换中,探头H面方向图对远区副瓣引入较大误差的情况,结合国内传统的E面电场法和K.T.Selvan提出的边缘电流逼近法各自的优点,利用混合算法研究了一种新的探头方向图逼近公式,并将其应用于平面近场测试中。通过在某大型微波暗室对一频段阵列天线进行实际测量,分别用E面电场法、边缘电流逼近法以及新的方法进行带探头补偿的近远场变换。最后,将各种方法与实际测试结果进行比较,求得其误差曲线,并在全域的角度分析各种方法的-50 d B超低副瓣精度。结果表明,此方法集合了前两种方法的优点,相比E面电场法,远区副瓣精度提高了8.2 d B,整个角域内副瓣精度提高了1.13 d B;相比边缘电流逼近法,近区副瓣精度提高了0.89d B,整个角域内副瓣精度提高了0.87d B。
基金supported by the National Natural Science Foundation of China (No.41276041)the NSFC–Shandong Joint Fund for Marine Science Research Centers (No.U1406404)
文摘Ten years （from 2005 to 2014） of satellite sea surface temperature （SST） data from the Advanced Very High Resolution Radiometer （AVHRR） are analyzed to reveal the monthly changes in surface cold patches （SCPs） in the main areas of the Northern Yellow Sea （NYS）. The Canny edge detection algorithm is used to identify the edges of the patches. The monthly changes are de- scribed in terms of location, temperature and area. The inter-annual variations, including changes in the location and area of the SCPs from 2010 to 2014, are briefly discussed. The formation mechanisms of the SCPs in different periods are systematically analyzed using both in situ data and numerical simulation. The results show that from May to October, the location and area of the SCPs re- main stable, with a north-south orientation. The SCPs altogether cover about I° of longitude （124°E-125°E） in width and 2° of lati- tude （37.5°N-39.5°N） in length. In November, the SCP separates from the Jangsan Cape and forms a closed, isolated, and approxi- mately circular cold patch in the central NYS. From May to October, the upweUing that leads to the formation of the SCP is mainly triggered by the headland residual current, wind field, climbing movement of the current and secondary circulation at the tide front. In November, cyclonic circulation in the NYS is primarily responsible for generating the upwelling that leads to the formation of the closed and isolated SCE
