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Volume 32 Issue 2
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Article Navigation >  Haiyang Xuebao  > 2010  >  32(2): 54-65
QU Wei-zheng, ZHU Xiao-jie, ZHAO Jin-ping, DU Ling, DENG Sheng-gui, HUANG Fei. Stimulation of the North Atlantic Oscillation by volcano activities[J]. Haiyang Xuebao, 2010, 32(2): 54-65.
Citation: QU Wei-zheng, ZHU Xiao-jie, ZHAO Jin-ping, DU Ling, DENG Sheng-gui, HUANG Fei. Stimulation of the North Atlantic Oscillation by volcano activities[J]. Haiyang Xuebao, 2010, 32(2): 54-65.
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Stimulation of the North Atlantic Oscillation by volcano activities

  • College of Environment Oceanography,China Ocen University of China, Qingdao 266100,China

  • Received Date: 2009-03-22
  • Rev Recd Date: 2009-08-27
    Abstract
  • Based on the correlation analysis and the analysis of vertical structure of temperature and geopotential field in Icelandic low and Azores high, we found that the Volcanic Explosive Index (VEI) anomaly for volcano eruption above category 5 shows negative correlation with sea level pressure (SLP) in Icelandic low, and positive correlation with SLP in Azores high. From the analysis of the vertical atmospheric structure, it is found that in summer, the Azores high is a deep warm core system and the Icelandic low is a shallow system. Therefore, the VEI shows negative correlation with the SLP in Azores high and positive correlation with SLP in Icelandic low. While in winter, the Azores high is a shallow system and the Icelandic low is a deep cold core system. Hence, the VEI shows positive correlation with the SLP in Azores high and negative correlation with SLP in Icelandic low. Considering the phase shift of the temperature and geopotential height field between summer and winter in Icelandic low and Azores high, the anomaly VEI causes opposite responses in the two circulation system, forms opposite phase SLP oscillation in middle and high latitude, and hence stimulated the famous North Atlantic Oscillation.
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