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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 - 映射技术在西格陵兰省杰克波瓦恩附近生成超透明熔岩库存

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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°C 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:我们分析了沿着格陵兰岛西海岸的Jakobshavn消融区域(JAR)的13年期间(2000-2012)的Landsat-7图像。此外,我们还使用FoveAPRO图像处理软件介绍了一种新的半自动技术,用于使用FoveAPRO图像处理软件(插入到Adobe Photoshop™),大大简化过程,并导致更精确的空间熔体犹太席克斯通过现有的手动方法。我们发现总平均熔融湖面积为0.30±0.12 km〜2(±1σ),最大熔化湖区域以研究期间的平均速度增加0.032 km〜2 d〜(-1)。此外,我们还注意到整体平均湖高程(每季〜200米〜200米)的每年季节性增加(〜1.8 md〜(-1)),以及最大的区域熔化湖泊〜1320±20m的最佳升高(±1σ)。我们还发现〜3.8m A〜(-1)(〜50米)的最大平均熔体升高(MAME)的增加。基于在附近的自动化气象站记录的数据,平均季节性温度在13年期间增加〜1.6°C,平均速率为0.125°C a〜(-1)。虽然温度是用于熔融水的驾驶员,但我们得出结论,与表面形貌相关的机制更可能调节消融区中熔体湖泊的空间图案和特征。

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