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MODIS observed increase in duration and spatial extent of sediment plumes in Greenland fjords

机译:MODIS观察到格陵兰峡湾沉积物羽流的持续时间和空间范围增加

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The freshwater flux from the Greenland Ice Sheet (GrIS) to the North Atlantic Ocean carries extensive but poorly documented volumes of sediment. We develop a suspended sediment concentration (SSC) retrieval algorithm using a large Greenland specific in situ data set. This algorithm is applied to all cloud-free NASA Moderate Resolution Imaging Spectrometer (MODIS) Terra images from 2000 to 2012 to monitor SSC dynamics at six river plumes in three fjords in southwest Greenland. Melt-season mean plume SSC increased at all but one site, although these trends were primarily not statistically significant. Zones of sediment concentration 50 mg Lsupa??1/sup expanded in three river plumes, with potential consequences for biological productivity. The high SSC cores of sediment plumes ( 250 mg Lsup−1/sup expanded in one-third of study locations. At a regional scale, higher volumes of runoff were associated with higher melt-season mean plume SSC values, but this relationship did not hold for individual rivers. High spatial variability between proximal plumes highlights the complex processes operating in Greenland's glacioa??fluviala??fjord systems.
机译:从格陵兰冰原(GrIS)到北大西洋的淡水通量携带着大量但记录不足的沉积物。我们使用大型格陵兰岛特定的原位数据集开发了悬浮泥沙浓度(SSC)检索算法。该算法已应用于2000年至2012年的所有无云NASA中分辨率成像光谱仪(MODIS)Terra图像,以监测格陵兰西南部三个峡湾中六条河羽的SSC动态。融化季节的平均羽流SSC在除一个站点外的所有站点都增加了,尽管这些趋势主要在统计上并不显着。沉积物浓度大于50 mg L a ?? 1 的区域在三个河羽中扩展,对生物生产力具有潜在的影响。三分之一的研究地点扩展了沉积物羽状流的高SSC核心(> 250 mg L &负; 1 )。值,但这种关系并不适用于个别河流,近端羽流之间的高度空间变异性突显了格陵兰冰川-fluviala-峡湾系统中的复杂过程。

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