| 1. | Absorbs infrared radiation ; affects tropospheric o
吸收红外线辐射，影响对流层中o |
| 2. | Low tropospheric wind profile from a 1 . 06 m doppler lidar
多普勒激光雷达的低对流层风场测量 |
| 3. | Forward propagation by tropospheric scatter
正向对流层散射传播 |
| 4. | Trapped mode tropospheric propagation
陷波模式对流层传播 |
| 5. | Current tropospheric concentration of n
现时在对流层的n |
| 6. | Storms severity index of severe convective weather in the middle and lower tropospheric jet
中低空急流带内的强对流天气的风暴强度指数 |
| 7. | Meantime , continuation of low tropospheric jet produces plentiful vapor for formation and continuation of rain gush
同时，低空西南急流的维持，为暴雨的产生和维持提供了充足的水汽。 |
| 8. | The results also show that saastamoinen / niell model can remove the most of the tropospheric delay , and then significantly improve the success rate and the reliability of ambiguity resolution . 4
结果显示，不论在模糊度解算的成功率和可靠性上，还是在计算速度上，加权最小二乘法都优于kalman滤波。 |
| 9. | Evaporation ducts , or tropospheric ducts in general , can guide radio waves to distances far beyond the horizon with less attenuation , and then severely impair some certain radio wave system
以蒸发波导为代表的对流层大气波导传播，可使电波在较小的衰减下沿波导传播得很远，从而严重影响合适的无线电系统。 |
| 10. | The ncep / ncar globally tropospheric 1 1 reanalysis data have been employed to select six landfall typhoon cases in order to diagnose variations of typhoon warm sectors in atmospheric boundary layer during their whole life periods
摘要采用ncep / ncar全球对流层1 1再分析格点资料，选取6个登陆台风个例，分析了不同发展阶段台风大气边界层暖区变化的特征及其与强度变化的关系。 |
