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《Journal of Glaciology and Geocryology》 2008-04
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The Relation between Daily Variation of Air Temperature and Surface Ablation in the Fair-Weather of Warm Season in 2006 on Qiyi Glacier,Qilan Mountains

HE Jian-qiao1,2,WANG Ning-lian1,JIANG Xi1,2,CHEN Liang1,2,SONG Gao-ju1,2,LI Quan-lian1,2,WU Xiao-bo1,2(1.State Key Laboratory of Cryospheric Sciences,CAREERI,CAS,Lanzhou Gansu 730000,China;2.Graduate University of Chinese Academy of Sciences,Beijing 100039,China)  
Surface ablation and meteorological factors had been monitored on the Qiyi Glacier in 2006.The results show that the daily variation of air temperature lags behind the ablation intensity in the fair weather of warm season and the phase difference between the two maximum values is about 4 h.By summarizing and analyzing the field data,the viewpoint is taken shape that the net radiation is a large proportion of the heat for ablation and ablation intensity does not coincide with air temperature,which is determined by the variation of net radiation.Local circulation influences intensively the air temperature of the glacierized region,and horizontal heat exchange between glacierized area and non-glacierized area and properties of underlying surface of the glacierized region determine the air temperature over the ablation area.
【Fund】: 中国科学院创新团队国际合作伙伴计划项目(CXTD-Z2005-2);; 国家重点基础研究发展计划项目(2005CB422003);; 国家杰出青年科学基金项目(40525001);; 中国科学院百人计划项目(2004401);; 中国科学院优秀人才项目(2005406)资助
【CateGory Index】: P343.6
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