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Volume 12 Issue 4

Oct.  1995

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 1995 >  12(4): 507-512

Condensation Induced by Rarefaction Waves and Reflected Rarefaction Waves

  • 1.

    Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026,Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026,Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026


doi: 10.1007/BF02657008

  • In this paper, homogeneous condensation induced by unsteady rarefaction waves and reflected rarefaction waves in vapor-gas mixture was investigated experimentally. It is shown that the temperature of condensation onset during very fast unsteady expansion in vapor-gas mixture is much lower than that during equilibrium process in the atmosphere. It is of interest to indicate that the size of droplets approximates a constant, but the number density and the mass density of droplets change rapidly in the region of static flow.
  • [1] LI Xiaofan, SHEN Xinyong, LIU Jia, 2014: Effects of Doubled Carbon Dioxide on Rainfall Responses to Large-Scale Forcing: A Two-Dimensional Cloud-Resolving Modeling Study, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 525-531.  doi: 10.1007/s00376-013-3030-2
    [2] Venkat NR. Mukku, 1990: The Ozone, Aerosol Depletion and Condensation Nuclei Events in the Stratosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 192-196.  doi: 10.1007/BF02919157
    [3] D.M. CHATE, RT. . WAGHMARE, C.K. JENA, V. GOPALAKRISHNAN, P. MURUGAVEL, Sachin D. GHUDE, Rachana KULKARNI, P.C. S. DEVARA, 2018: Cloud Condensation Nuclei over the Bay of Bengal during the Indian Summer Monsoon, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 218-223.  doi: 10.1007/s00376-017-6331-z
    [4] Zheng Weizhong, Yu Zhihao, 1987: THE EFFECTS OF FRICTION AND HEATING OF CONVECTTVE CONDENSATION IN THE BAROCLINIC INSTABILITY PROBLEM, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 447-459.  doi: 10.1007/BF02656744
    [5] Xiaofei LI, Qinghong ZHANG, Huiwen XUE, 2017: The Role of Initial Cloud Condensation Nuclei Concentration in Hail Using the WRF NSSL 2-moment Microphysics Scheme, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1106-1120.  doi: 10.1007/s00376-017-6237-9
    [6] Jiefan YANG, Hengchi LEI, Yuhuan LÜ, 2017: Airborne Observations of Cloud Condensation Nuclei Spectra and Aerosols over East Inner Mongolia, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 1003-1016.  doi: 10.1007/s00376-017-6219-y
    [7] Jun ZHANG, Jiming SUN, Wei DENG, Wenhao HU, Yongqing WANG, 2023: The Importance of the Shape Parameter in a Bulk Parameterization Scheme to the Evolution of the Cloud Droplet Spectrum during Condensation, ADVANCES IN ATMOSPHERIC SCIENCES, 40, 155-167.  doi: 10.1007/s00376-022-2065-7
    [8] LI Jun, CHEN Hongbin, Zhanqing LI, WANG Pucai, Maureen CRIBB, FAN Xuehua, 2015: Low-Level Temperature Inversions and Their Effect on Aerosol Condensation Nuclei Concentrations under Different Large-Scale Synoptic Circulations, ADVANCES IN ATMOSPHERIC SCIENCES, 32, 898-908.  doi: 10.1007/s00376-014-4150-z
    [9] Sarbari Ghosh, Utpal Kumar De, 1997: A Comparative Study of the Atmospheric Layers below First Lifting Condensation Level for Instantaneous Pre-Monsoon Thunderstorm Occurrence at Agartala (23o30’N, 91o15’E) and Ranchi (23o14’N, 85o14’E) of India, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 93-102.  doi: 10.1007/s00376-997-0048-3
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    [11] Xiaofan Li, Han-Ru Cho, 1997: Development and Propagation of Equatorial Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 14, 323-338.  doi: 10.1007/s00376-997-0053-6
    [12] Zhang Xuehong, Zeng Qingcun, Bao Ning, 1986: NONLINEAR BAROCLINIC HAURWITZ WAVES, ADVANCES IN ATMOSPHERIC SCIENCES, 3, 330-340.  doi: 10.1007/BF02678653
    [13] Yong. L. McHall, 1991: Planetary Stationary Waves in the Atmosphere Part I: Orographic Stationary Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 211-224.  doi: 10.1007/BF02658095
    [14] Yong. L. McHall, 1991: Planetary Stationary Waves in the Atmosphere Part II: Thermal Stationary Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 8, 225-236.  doi: 10.1007/BF02658096
    [15] Liu Shida, Liu Shikuo, 1990: Advances in Studies on Nonlinear Atmospheric Waves, ADVANCES IN ATMOSPHERIC SCIENCES, 7, 227-244.  doi: 10.1007/BF02919161
    [16] Chen Zhongming, Liu Fuming, Li Xiaoping, Tao Jie, 1994: Oscillatory Rossby Solitary Waves in the Atmosphere, ADVANCES IN ATMOSPHERIC SCIENCES, 11, 65-73.  doi: 10.1007/BF02656995
    [17] CHEN Gong, and LI Guoping, 2014: Dynamic and Numerical Study of Waves in the Tibetan Plateau Vortex, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 131-138.  doi: 10.1007/s00376-013-1035-5
    [18] Tianju WANG, Zhong ZHONG, Ju WANG, 2018: Vortex Rossby Waves in Asymmetric Basic Flow of Typhoons, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 531-539.  doi: 10.1007/s00376-017-7126-y
    [19] Qin XU, Wei GU, GAO Shouting, 2005: Nonlinear Oscillations of Semigeostrophic Eady Waves in the Presence of Diffusivity, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 49-57.  doi: 10.1007/BF02930869
    [20] Sun Shuqing, 1985: GRAVITY WAVES ON THE AXIS OF LOW LEVEL JET AND THEIR INSTABILITY, ADVANCES IN ATMOSPHERIC SCIENCES, 2, 112-123.  doi: 10.1007/BF03179743
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    • Manuscript History

    Manuscript received: 10 October 1995
    Manuscript revised: 10 October 1995
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    Condensation Induced by Rarefaction Waves and Reflected Rarefaction Waves

    • 1. Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026,Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026,Department of Modern Mechanics University of Science and Technology of China, Hefei, Anhui 230026
    • Manuscript received: 1995-10-10
    • Manuscript revised: 1995-10-10

    Abstract: In this paper, homogeneous condensation induced by unsteady rarefaction waves and reflected rarefaction waves in vapor-gas mixture was investigated experimentally. It is shown that the temperature of condensation onset during very fast unsteady expansion in vapor-gas mixture is much lower than that during equilibrium process in the atmosphere. It is of interest to indicate that the size of droplets approximates a constant, but the number density and the mass density of droplets change rapidly in the region of static flow.

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