利用低轨道卫星间微波信号探测反演温湿廓线

通过同时测量微波信号的折射和吸收信息，低地球轨道卫星间（LEO-LEO）微波掩星探测技术能够独立反演温度和水汽廓线。通过仿真手段，首先，正演模拟了微波信号穿过大气层后由折射和吸收效应分别导致的相位延迟和振幅衰减，在此基础上，对温度、水汽和云中液态水反演廓线进行了个例分析，然后，统计分析了温度和水汽在不同纬度带的反演性能，以及云对反演精度的影响。结果表明：温度在约35 km以上存在明显正偏差，高纬度的最大，中纬度次之，低纬度最小。水汽反演误差在约4 km以下明显增大，低纬度的最大，中纬度次之，高纬度最小。有云存在时，需要去除云的吸收作用，否则温度和水汽会出现明显的正偏差。上述研究为进一步发展LEO-LEO掩星探测计划提供了理论参考依据。     

On the Stark broadening of the Re II spectral lines

Stark broadening parameters - full widths at half maximum (FWHM) and shifts for 11 Re II lines have been calculated. The plasma parameters used were electron density of ${10}^{17}$ cm^?3 and temperature from 5 000 K to 80 000 K. Calculations were performed using the simplified modified semiempirical (SMSE) approach and compared with calculations by Cowley’s approximative Stark broadening formula at 10000 K, usefull in spectrum synthesis. The results have also been considered in the atmosphere model of A type star and for DB white dwarfs.