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Volume 21 Issue 3
Jun 2010
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Journal of Earth Science  > 2010  >  21(3): 272-283.
Weizheng QU, Shenggui DENG, Fei HUANG, Yingchen LIU, Ting FAN, Yan BAI. Effect of volcanic activities and CO2 concentration on summer temperature in middle stratosphere, North Hemisphere. Journal of Earth Science, 2010, 21(3): 272-283. doi: 10.1007/s12583-010-0091-3
Citation: Weizheng QU, Shenggui DENG, Fei HUANG, Yingchen LIU, Ting FAN, Yan BAI. Effect of volcanic activities and CO2 concentration on summer temperature in middle stratosphere, North Hemisphere. Journal of Earth Science, 2010, 21(3): 272-283. doi: 10.1007/s12583-010-0091-3
shu

Effect of volcanic activities and CO2 concentration on summer temperature in middle stratosphere, North Hemisphere

doi: 10.1007/s12583-010-0091-3

  • Department of Marine Meteorology, Ocean University of China, Qingdao, 266100, China

Funds:

the National Natural Science Foundation of China 40875041

the National Natural Science Foundation of China 40631006

the National Natural Science Foundation of China 40975038

More Information
  • Corresponding author: Weizheng QU: quweizhe@ouc.edu.cn
  • Received Date: 03 Aug 2009
  • Accepted Date: 20 Nov 2010
  • Publish Date: 01 Jun 2010
    Abstract
  • Successive filtration and comparison show that the stratosphere air temperature in 10 hPa-layer of the Northern Hemisphere (NH) in July continuously increases, which is associated to the increases in greenhouse gases mostly CO2, volcanic activities, and solar activity, demonstrating the follows. (a) The increase in CO2 concentration is largely consistent with that of the stratosphere air temperature in 10 hPa-layer of the NH in July. However, the increase in the air temperature is not in a linear pattern, during which several cooling events interrupt. The cooling events between late 1960s and late 1970s are remarkable ones and so is the one before mid 1990s. Analysis shows that these events are induced by volcanic activities and solar activity. (b) The CO2-free variation in the stratosphere air temperature in 10 hPa-layer of the NH is consistent with that of the solar magnetic index. The wave crests and wave troughs of the two curves are consistent in phase, and the curve of solar magnetic index leads the other slightly. In other words, when the solar magnetic pole is southward, a warming in the NH stratosphere corresponds; and on the contrary, the northward solar magnetic pole corresponds to a cooling event. The variation in solar magnetic polarity strongly impacts the variation in the stratosphere temperature.

     

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