Model simulation of the amount of soluble mass during cloud droplet formation

被引:10
|
作者
Korhonen, P
Kulmala, M
Vesala, T
机构
关键词
condensation; cloud droplet activation; nitric acid;
D O I
10.1016/1352-2310(95)00380-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The development of the amount of hygroscopic material from nitric acid vapour in nascent cloud droplets has been studied. This phenomenon was approached first by simple calculations in order to find out maximum values of condensed hygroscopic material in droplets and in cloud water. Then, a more detailed parcel model with the binary condensation of water and nitric acid vapours was used for the simulations of the development of droplet distribution and the composition of droplets. In the parcel model vapours are condensing on the ammonium nitrate particles. According to the results of this study condensation of nitric acid could increase considerably the amount of nitrate ions in the droplets, if we compare this to the amount of nitrate ions from ammonium nitrate salt. This can lead to the enhanced amount of activated cloud droplets.
引用
收藏
页码:1773 / 1785
页数:13
相关论文
共 50 条
  • [41] A DIRECT NUMERICAL SIMULATION EXPERIMENT OF CLOUD DROPLET GROWTH BY ACCRETION
    KORNFELD, P
    SHAFRIR, U
    DAVIS, MH
    BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 1968, 49 (5P2) : 596 - &
  • [42] Activation barrier for multicomponent droplet formation on partially soluble nuclei
    Djikaev, YS
    Donaldson, DJ
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D13): : 14447 - 14463
  • [43] Initial cloud droplet number concentrations in clean and polluted areas: Simulation by a condensation model and comparison with measurements
    Seidl, Winfried
    ATMOSPHERIC RESEARCH, 1994, 31 (1-3) : 157 - 185
  • [44] Aerosol-landscape-cloud interaction: signatures of topography effect on cloud droplet formation
    Romakkaniemi, Sami
    Maalick, Zubair
    Hellsten, Antti
    Ruuskanen, Antti
    Vaisanen, Olli
    Ahmad, Irshad
    Tonttila, Juha
    Mikkonen, Santtu
    Komppula, Mika
    Kuhn, Thomas
    ATMOSPHERIC CHEMISTRY AND PHYSICS, 2017, 17 (12) : 7955 - 7964
  • [45] THE INFLUENCE OF AEROSOL-PARTICLE COMPOSITION ON CLOUD DROPLET FORMATION
    HALLBERG, A
    OGREN, JA
    NOONE, KJ
    OKADA, K
    HEINTZENBERG, J
    SVENNINGSSON, IB
    JOURNAL OF ATMOSPHERIC CHEMISTRY, 1994, 19 (1-2) : 153 - 171
  • [46] MECHANISMS OF FORMATION OF BIMODAL CLOUD DROPLET SPECTRA IN STRATIFORM CLOUDS
    KOROLEV, AV
    IZVESTIYA AKADEMII NAUK FIZIKA ATMOSFERY I OKEANA, 1992, 28 (10-11): : 1044 - 1053
  • [47] Cloud droplet spectra formation by ripening process with internal mixing
    Çelik, F
    CONFERENCE ON CLOUD PHYSICS, 1998, : J21 - J23
  • [48] Cloud condensation nuclei and cloud droplet measurements during ACE-2
    Snider, JR
    Brenguier, JL
    TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY, 2000, 52 (02): : 828 - 842
  • [49] A MODEL OF THE DEVELOPMENT OF DROPLET EFFECTIVE RADIUS IN CONVECTIVE CLOUD
    CHOULARTON, TW
    BOWER, KN
    QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1993, 119 (511) : 443 - 456
  • [50] Soluble mass, hygroscopic growth, and droplet activation of coated soot particles during LACIS Experiment in November (LExNo)
    Henning, S.
    Wex, H.
    Hennig, T.
    Kiselev, A.
    Snider, J. R.
    Rose, D.
    Dusek, U.
    Frank, G. P.
    Poeschl, U.
    Kristensson, A.
    Bilde, M.
    Tillmann, R.
    Kiendler-Scharr, A.
    Mentel, T. F.
    Walter, S.
    Schneider, J.
    Wennrich, C.
    Stratmann, F.
    JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115