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Analysis of the temperature dynamics of a proglacial river using time-lapse thermal imaging and energy balance modeling

机译:基于延时热成像和能量平衡模型的冰河温度动态分析

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摘要

Understanding the temperature dynamics of rivers is critical for their management and for ecological and biogeochemical aquatic processes. In proglacial rivers, there is typically a paucity of thermal observations which in turn limits the understanding of these sensitive and evolving environments. Here we collected ground-based thermal images, with approximately meter resolution and imaged every half hour for 24 h, of a proglacial river and 2 km(2) of its floodplain and interpret the observations using a numerical energy balance model. The images revealed the longitudinal thermal pattern of the Urbach River in Switzerland there was gradual cooling in the upstream half of the study section and then warming in the remaining downstream portion. This pattern persisted through the diurnal warming and cooling cycle. The spatio-temporal thermal pattern was explained by a model that included distributed thermal inputs of cooler water in the upstream half coming from alluvial fans and warmer water in the downstream half running off steep cliffs that warm snowmelt. The warm inputs from the cliffs were confirmed by the thermal imaging. These data and the associated modeling illustrated that distributed inflows can overwhelm the influence of atmospheric fluxes, and that their knowledge is critical for understanding stream temperatures. The combination of modeling and detailed time-lapse thermal imaging allowed for identification and quantification of processes critical to in-stream temperature dynamics in a proglacial river. (C) 2014 Elsevier B.V. All rights reserved.
机译:了解河流的温度动态对于河流的管理以及生态和生物地球化学水生过程至关重要。在冰河河流中,通常缺乏热观测资料,这反过来又限制了对这些敏感和不断变化的环境的理解。在这里,我们以大约米的分辨率收集了地面热图像,每半小时对一条冰川河和其洪泛区2 km(2)进行成像,并使用数值能量平衡模型解释了观测结果。图像显示了瑞士乌尔巴赫河的纵向热模式,研究段的上游部分逐渐冷却,然后在其余下游部分逐渐变暖。这种模式在昼夜升温和降温周期中一直存在。时空热模式由一个模型解释,该模型包括来自冲积扇的上游一半的较冷水和下游一半的较热水(分布在陡峭的悬崖上,使融雪变暖)的分布式热输入。来自悬崖的热输入已通过热成像确认。这些数据和相关的模型说明,分布的入流可以压倒大气通量的影响,并且它们的知识对于理解河流温度至关重要。建模与详细的延时热成像相结合,可以识别和量化对冰川河流中河内温度动态至关重要的过程。 (C)2014 Elsevier B.V.保留所有权利。

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