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2014年12月-2015年4月期间,新疆布尔津县喀纳斯湖举行了冰上旅游项目.为监测冰层生长、发育和融化状况,分别对喀纳斯湖(湖边、湖中)A、B、C三点进行温度监测,利用监测得到的冰层温度数据绘制湖冰从上到下温度分布状况图.根据湖边与湖中的冰层结构特点,从冰层的天然结构角度分析湖冰结构对温度分布的影响.结果表明:天然冰层中温度传递系数并不是一致不变的,既受冰上气温、冰下湖水温度的影响,也受到冰层自身结构状况的影响,并进一步阐述了湖面冰层的温度分布规律与变化成因,为分析温度对冰层强度的影响奠定了基础.
Ice-skating tourism was held in Kanas Lake, Burqin County, Xinjiang from December 2014 to April 2015. In order to monitor the growth, development and thawing of ice sheets, A, B, C three points of temperature monitoring, the use of monitoring the ice temperature data to draw the ice lake top-down temperature distribution map.According to the lakeside and lake ice structure characteristics, from the natural structure of the ice point of view The results show that the temperature transfer coefficient in the natural ice is not consistent, and is affected not only by the ice temperature, the temperature of the ice under the ice, but also by the structure of the ice itself, And further elaborated the lake ice temperature distribution law and causes of change, which laid the foundation for analyzing the influence of temperature on the ice strength.