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Coordinated MST radar and lidar observations for the study of mesospheric structures over a tropical station

机译:MST雷达和激光雷达观测的协调观测,用于研究热带台站的中层结构

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VHF radar observations at a frequency of 53 MHz at Gadanki (13.5°N, 79.2°E), India, during the period from September 1995 to August 1999 are used to study the tropical mesospheric structures. MST radar echoes have shown an enhancement in echo power of about 6-8 dB above the average noise level. These echoes are intermittent in time and can be observed at an altitude between 70 and 76 km. The seasonal variation of these echoes shows the maximum percentage occurrence during summer, closely followed by equinoxes and minimum during winter. This seasonal variation is also accompanied by shifting of height to lower heights during winter. Coordinated MST radar and Nd:YAG lidar observations were conducted to study the mesospheric structures during March 1998-June 1999. In the lidar temperature profiles, inversion of about 20-30 K is observed at the heights of the MST radar-enhanced echoes. Enhanced radar reflectivity is observed on both the preceding and succeeding days of lidar observations of strong temperature inversions. Percentage occurrence of MST radar echoes and temperature inversions show one-to-one correspondence for most of the cases. The effect of temperature inversion on the radar reflectivity is also studied. The presence of temperature inversion and enhanced radar reflectivity are discussed in the light of gravity-wave breaking processes at that height region.
机译:1995年9月至1999年8月期间,在印度Gadanki(13.5°N,79.2°E)以53 MHz的频率进行甚高频雷达观测,用于研究热带中层结构。 MST雷达回波显示出回波功率比平均噪声水平高出约6-8 dB。这些回声在时间上是断断续续的,可以在70至76 km的高度观察到。这些回声的季节变化表明,夏季最大百分比发生,紧接着是春分点,冬季最小。这种季节性变化还伴随着冬季时身高向低身的转变。在1998年3月至1999年6月期间,对MST雷达和Nd:YAG激光雷达进行了协调观测,以研究中层结构。在激光雷达温度剖面中,在MST雷达增强回波的高度观测到约20-30 K的反演。在强温度反转的激光雷达观测的前几天和后几天都观察到增强的雷达反射率。在大多数情况下,MST雷达回波和温度反演的发生率显示一一对应。还研究了温度反演对雷达反射率的影响。根据该高度区域的重力波分解过程,讨论了温度反转和雷达反射率提高的问题。

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