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声雷达探测与直接测量温度结构系数的对比研究 被引量:2

A COMPARATIVE STUDY BETWEEN THE TEMPERATURE STRUCTURE COEFFICIENTS DETECTED BY SODAR AND DIRECT METHODS
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摘要 本文用对比方法研究声雷达定量探测温度结构系数的接收因子和衰减因子,分析了接收因子与某些气象要素的关系。分析结果表明,在63米高度上接收因子E=CT,a2/CT,d2与局地稳定度有关,它随稳定度的增大而增大;E值大小还与水汽量有关,E随水汽量的增大而增大;E值大小还与高度有关,它随高度增大而减小。分析结果还表明,在稳定条件下,衰减因子LE(E160/E63)的大小与160米高度上的水平风速有关,它随风速的增大而增大。文中还对气象条件对声雷达定量探测温度结构系数的影响进行了讨论。 The receiving factor and the attenuation factor of temperature structure coefficients detected by sodar are studies by comparative method. The analytical results show that the receiving factor E-CT,a2/CT,d2 at height 63m is related to local stability, and it increases with increase of stability. The receiving factor E is related to water vapor as well, it increases with increase of water vapor. The attenuation factor (LE= E160/E63) is related to horizontal wind velocity at 160m under stable condition. It is increased with increase of horizontal wind velocity. Finally, effects of meteorological factors on temperature structure coefficient detected by sodar are discussed.
出处 《地球物理学报》 SCIE EI CAS 1982年第6期492-499,共8页 Chinese Journal of Geophysics
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同被引文献7

  • 1章基嘉 朱抱真.青藏高原气象学进展[M].北京:科学出版社,1988.78-88.
  • 2曲绍厚 宋锡铭 等.北京城市气象效应[J].地球物理学报,1981,24(3):229-237.
  • 3周明煜 吕乃平.大气对流边界层热力湍流过程的研究[J].气象学报,1987,45(4):451-458.
  • 4Zhou Mingyu,大气科学,1985年,42卷,1期,47页
  • 5周明煜,地球物理学报,1982年,25卷,4期,492页
  • 6曲绍厚,地球物理学报,1981年,24卷,3期,229页
  • 7Zhou Mingyu,Acoustic Soc Am,1980年,68卷,1期,303页

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