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Monitoring ice-capped active Volćan Villarrica, southern Chile, using terrestrial photography combined with automatic weather stations and global positioning systems

机译:结合地面摄影,自动气象站和全球定位系统,监测智利南部活跃的冰封火山VolćanVillarrica

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摘要

Volcán Villarrica (39°25'12?S, 71°56'27?W; 2847 m a.s.l.) is an active ice-capped volcano located in the Chilean lake district. The surface energy balance and glacier frontal variations have been monitored for several years, using automatic weather stations and satellite imagery. In recent field campaigns, surface topography was measured using Javad GPS receivers. Daily changes in snow-, ice- and tephra-covered areas were recorded using an automatic digital camera installed on a rock outcrop. In spite of frequently damaging weather conditions, two series of consecutive images were obtained, in 2006 and 2007. These photographs were georeferenced to a resampled 90 m pixel size SRTM digital elevation model and the reflectance values normalized according to several geometric and atmospheric parameters. The resulting daily maps of surface albedo are used as input to a distributed glacier-melt model during a 12 day mid-summer period. The spatial pattern of cumulative melt is complex and controlled by the distribution of airfall and wind-blown tephra, with extremely high melt rates occurring downwind of the crater and exposed ash banks. The camera images are also used to visualize the pattern of glacier crevassing. The results demonstrate the value of terrestrial photography in understanding the energy and mass balance of the glacier, including the generation of meltwater, and the potential value of the technique for monitoring volcanic activity and potential hazards associated with ice-volcano interactions during eruptive activity.
机译:沃尔坎·比利亚里卡(VolcánVillarrica)(39°25'12?S,71°56'27?W; 2847 m a.s.l.)是一座活跃的冰封火山,位于智利湖区。利用自动气象站和卫星图像已经监测了表面能平衡和冰川正面变化多年。在最近的野战中,使用Javad GPS接收器测量了表面地形。使用安装在岩石露头上的自动数码相机记录雪,冰和特非拉覆盖区域的每日变化。尽管天气条件经常造成破坏,但在2006年和2007年仍获得了两个系列的连续图像。这些照片均经过地理重采样到重新采样的90 m像素大小SRTM数字高程模型,并且根据几个几何和大气参数对反射率值进行了归一化。所得的每日表面反照率图在仲夏12天期间用作分布式冰川融化模型的输入。累积熔体的空间格局是复杂的,并且受空降和吹制的特非拉风的分布控制,极高的熔体率发生在火山口和裸露的灰烬顺风处。摄像机图像还用于可视化冰川起皱的模式。结果表明,地面摄影对于了解冰川的能量和质量平衡(包括融化水的产生)的价值,以及监测火山活动和喷发活动期间与冰火山相互作用相关的潜在危害的技术的潜在价值。

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