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Snow algae in a Himalayan ice core: new environmental markers for ice-core analyses and their correlation with summer mass balance

机译:喜马拉雅冰芯中的雪藻:冰芯分析的新环境标志物及其与夏季质量平衡的相关性

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摘要

Snow algae in a shallow Ice core (6.98 m long) from Yala glacier in the Langtang region of Nepal were examined for potential use as environmental markers in ice-core analysis. The ice core, taken at 5350ma.s.l. in 1994, was estimated to contain 11 annual layers from 1984 to 1994 from the profile of algal biomass. Algal biomass in each annual layer was noted to be correlated with air temperature, and the following two environmental indices which were calculated from air temperature and precipitation at Kyangjing (3920ma.s.L), the village nearest to Yala glacier: estimated mean snow-cover thickness (MST) and estimated summer mass balance (SMB). Both parameters reflect snow-cover thickness on algal layers, which would be a major determinant of the light available for algal growth on the glacier. Snow algal biomass in the ice core appears to be a good environmental marker for indicating air temperature and accumulation during summer, which is important for understanding the mass balance of summer-accumulation-type glaciers in this region.
机译:检查了尼泊尔朗塘地区亚拉冰川浅冰芯(长6.98 m)中的雪藻,可作为冰芯分析中的环境标志物。冰芯,摄于5350ma.s.l。根据藻类生物量的分布,在1994年到1984年至1994年期间,估计每年包含11个年度层。注意到每一年层中的藻类生物量都与气温相关,以下两个环境指数是根据距离雅拉冰川最远的村庄Kyangjing(3920ma.sL)的气温和降水计算得出的:估计的平均积雪厚度(MST)和估计的夏季质量平衡(SMB)。这两个参数都反映了藻层上的积雪厚度,这将是可用于冰川上藻类生长的光的主要决定因素。冰芯中的雪藻生物质似乎是指示夏季气温和积聚的良好环境标志,这对于了解该地区夏季积聚型冰川的质量平衡非常重要。

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