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首页> 外文期刊>Polar Geography >Generating a supraglacial melt-lake inventory near Jakobshavn, West Greenland, using a new semi-automated lake-mapping technique
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Generating a supraglacial melt-lake inventory near Jakobshavn, West Greenland, using a new semi-automated lake-mapping technique

机译:使用新的半自动湖泊映射技术在西格陵兰岛雅各布沙文附近生成冰川上融化湖水清单

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We analyze Landsat-7 imagery spanning a 13-year period (2000-2012) for the Jakobshavn Ablation Region (JAR) along the west coast of Greenland. In addition, we introduce a new semi-automated technique for the mapping of melt-lakes using FoveaPro image-processing software (plug-in to Adobe Photoshop™), greatly simplifying the process, and resulting in more-precise spatial melt-lake statistics over existing manual methods. We found a total mean melt-lake area of 0.30±0.12 km~2 (±1σ), with maximum melt-lake area increasing at an average rate of 0.032 km~2 d~(-1) across the study periods. Additionally, we note a yearly seasonal increase (~1.8 m d~(-1)) in the overall mean lake elevation (~200 m per season) as well as an optimal elevation of the largest-area melt-lakes of ~1320±20m (±1σ). We also found an increase in the maximum average melt-lake elevation (MAME) of ~3.8 m a~(-1) (~50 m). Based on data recorded at nearby automated weather stations, the mean seasonal temperature increased ~1.6℃ over the 13-year period at an average rate of 0.125° C a~(-1). Although temperature is a driver for meltwater production, we conclude that mechanisms related to the surface topography are more likely modulating the spatial pattern and characteristics of melt lakes in the ablation zone.
机译:我们分析了格陵兰岛西海岸的雅各布港消融区(JAR)跨13年(2000-2012年)的Landsat-7影像。此外,我们采用FoveaPro图像处理软件(Adobe Photoshop™的插件)引入了一种新的半自动化技术,用于融化湖的制图,大大简化了过程,并获得了更精确的空间融化湖统计数据超过现有的手动方法。我们发现整个研究期间平均总融湖面积为0.30±0.12 km〜2(±1σ),最大融湖面积以平均0.032 km〜2 d〜(-1)的速率增加。此外,我们注意到整个湖面平均高程(每个季节〜200 m)的年度季节性增加(〜1.8 md〜(-1))以及最大区域融化湖的最佳高度〜1320±20m (±1σ)。我们还发现最大平均融湖高程(MAME)增加了〜3.8 m a〜(-1)(〜50 m)。根据附近自动气象站记录的数据,在13年中,平均季节性温度以平均0.125°C a〜(-1)的速度升高了约1.6℃。尽管温度是熔体水生产的驱动力,但我们得出的结论是,与表面形貌有关的机制更有可能调节消融区熔体湖的空间格局和特征。

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