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中文摘要：
以1992～2010年横断山区16个观测站土壤相对湿度资料为基础,通过Kriging插值法分析土壤相对湿度季节分异和空间分异特征。结果表明：横断山区年土壤相对湿度自1992年以来整体呈波动增加趋势,年际变化倾向率为0.51%/a;横断山区土壤相对湿度表现为西南和东北部较高,东南和西北部较低,中部土壤相对湿度增加趋势强于边缘,深层土壤的相对湿度整体大于浅层土壤。春、夏季土壤相对湿度增加趋势比秋、冬季明显。
英文摘要：
Based on soil relative moisture data in ten days from 16 observation stations of Hengduan Mountain- ous Region in 1992-2010, spatial and temporal changes of soil relative moisture were analyzed in the paper with Kriging interpolation method. The results showed that the soil relative moisture in Hengduan Mountain- ous Region had been in a increasing tendency since 1992 with the inclination rate of 0.5 l%/a. The soil relative moisture were high relatively in＂ the southwest and the northeast of Hengduan Mountains whereas low in the southeast and the northwest. The values of soil relative moisture in deep soils were higher than that in shallow soil. As far as the seasonal change, the increasing trend of soil relative moisture in spring and summer were greater than that in autumn and winter.
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The Surface Energy Budget in the Accumulation Zone of the Laohugou Glacier No. 12 in the Western Qil
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