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Interdecadal and decadal variation of temperature over north pole area and the relation with solar activity

Acta Oceanologica Sinica 2011年第2期30卷 53-61页

作者： QU Weizheng ZHAO Jinping DU Ling HUANG Fei FAN Tingting OceanUniversityofChina Qingdao266003China

Obvious tendency and periodicity of the air temperature can be detected over the north pole *** are reflected as follows： *** air temperature at the earth surface and in the middle layer of the stratosphere tends to be increased either in winter or in *** air temperature has increased 1.3 °C for about 50 years at a speed about 0.025 °C/year in January,and 0.013 °C/year in *** air temperature in the middle layer of the stratosphere （10 hPa） in January has increased 10 °*** temperature rising speed in July is 0.14 °C/*** speaking,the temperature rising speed is quicker in winter than in summer and quicker in the upper layer than at the earth *** air temperature at the top layer of the troposphere （100 hPa） over the north pole area tends to be increased either in winter or in *** air temperature in January has decreased 5.0 °C for about 50 years at a temperature decreasing speed about 0.094 °C/year,and at a temperature decreasing speed about 0.032 °C/year in *** speed of the temperature decreasing is greater in winter than in *** air temperature respectively at different altitudes over the north pole possesses interdecadal variation with a period of 22 *** July the amplitude of the variation with a period of 22 years decreases rapidly from the high altitude to the *** means that the 22–year’s period is more obvious at the high altitude than at the low *** the earth surface layer in north pole there also is obvious decadal variation with a period of 11 *** analysis indicates that the 22-years’ period temperature variation is associated with the periodic variation of the solar magnetic *** 11-year period temperature variation is corresponding to 11 year’ period of the variation of the sunspot number.

关键词： decadal variation of air temperature solar activity north pole area

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