在冰川学研究中,根据冰川活动层的水热状态,将冰川自上而下划为干雪带、渗浸带、附加冰带和消融带,其中,渗浸带是冰川同环境进行能量与物质交换强烈,内部水热输送最剧烈的一个带。此外,在渗浸带内部的水热输运过程中伴随着一系列渗浸冻结、渗浸成冰、雪层变质等成冰运动。对于该带向大气的吸热以及自身内部温度变化过程的了解,有助于全面地认识 In the research of glaciology, glaciers are classified as dry snow zone, infiltration zone, additional ice zone and ablation zone according to the hydrothermal state of the glacial activity layer. Among them, the infiltration zone is the relationship between the glacier’s energy and environment Strong physical exchange, the most intense internal water and heat transport zone. In addition, during the hydrothermal transport within the infiltration zone, a series of ice-forming movements, such as infiltration and freezing, infiltration and ice formation, and snow degeneration, are accompanied. Understanding the process of absorbing heat to the atmosphere and its own internal temperature changes helps to fully understand