通过初步分析认为，太阳活动是引起青藏高原地面加热场强度变化的重要原因之一。
Through the primary analyzing, we think that the sun activity is to cause the one of the important reasons of surface heating field change over QXP.
利用1982 ~ 1996年每天两次的NCEP再分析资料，研究青藏高原地面加热场的日变化对亚洲季风区环流的影响。
The impact of the diurnal variation of the surface heating in the Tibetan Plateau on the circulation over the Asian monsoon region is analyzed using the twice daily NCEP data from 1982 to 1996.
太阳黑子周期长度（SCL）变长（太阳活动减弱）时，青藏高原地面加热场强度减弱。
The surface heating fields over QXP die down when sunspot cycle length(SCL) become long(the sun activity die down).
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