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首页> 外文期刊>Environmental Monitoring and Assessment >Long-term mass balance modelling (1986-2018) and climate sensitivity of Siachen Glacier, East Karakoram
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Long-term mass balance modelling (1986-2018) and climate sensitivity of Siachen Glacier, East Karakoram

机译:长期大规模平衡造型(1986-2018)和SIACHEN冰川的气候敏感性,东喀喇昆仑

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Located in the eastern lap of the Karakoram Range, the Siachen Glacier is the second longest glacier in the non-polar areas of the world. High altitude, extreme climate and frequent military conflicts on this glacier create antagonistic surroundings for conventional field studies. Although recent advancements in geodetic technique have helped in the estimation of Siachen mass budget (MB), these geodetic estimates have been observed only for short time periods ranging 6 to 10 years. Hence, current study presents a comprehensive assessment of the Siachen long-term MB (32 years) based on temperature index (TI) model. Annual surface MB variability was modelled between 1986 and 2018 by forcing daily air temperature and precipitation from multiple ground stations distributed well across accumulation/ablation zone of the glacier. Mean annual temperature lapse rate (LR) was found midway between dry adiabatic and moist adiabatic LRs. Precipitation gradient (PG) was observed remarkably different below and above 4800 m.a.s.l. glacier altitude. Furthermore, snowmelt factor (SMF) was also estimated using snow thickness and positive degree days (PDDs) information over the glacier surface. Model results showed a nearly balanced condition (- 0.02 +/- 0.05 m.w.e./year) during 1986-2006 followed by an accelerated rate of mass loss during 2007-2018 (- 0.11 +/- 0.05 m.w.e./year), thus making the overall condition of Siachen MB negative during the period 1986-2018 (- 0.05 +/- 0.05 m.w.e./year). Comparison of modelled MB was made with few geodetic studies conducted for the Siachen Glacier at different time scales (mainly after year 2000). Further, the sensitivity of the modelled glacier-wide MB was - 0.24 m.w.e./year for a temperature rise by 1 degrees C, while the sensitivity towards 10% increase in precipitation was estimated to be + 0.16 m.w.e./year. A relationship of the annual MB with accumulation area ratio (AAR) and equilibrium line altitude (ELA) was also established for Siachen glacier.
机译:位于喀喇昆仑的东圈系列,SIACHEN冰川是世界上非极地冰川的第二次冰川。这款冰川的高海拔,极端气候和频繁的军事冲突会为传统的野外研究创造敌人的环境。虽然大地测量技术的最新进展有助于估计SIACHEN批准(MB),但这些大地测量估计仅在短时间内延伸到6至10年。因此,目前的研究提出了基于温度指数(TI)模型的SIACHEN长期MB(32岁)的全面评估。通过迫使日常的空气温度和来自多个地面站的沉淀在冰川的积累/消融区分布井之间的日常空气温度和降水,在1986和2018之间进行了建模的年度表面MB变异性。平均年度温度流逝率(LR)在干燥绝热和潮湿的绝热LRS之间发现。沉淀梯度(pG)在低于4800 m.a.1以上的显着不同观察到。冰川高度。此外,还使用冰川表面上的雪厚度和正度天(PDDS)信息来估算雪花尺寸(SMF)。模型结果在1986-2006期间显示了几乎平衡的条件( - 0.02 +/- 0.05 mWE /年),然后加速了2007 - 2018年( - 0.11 +/- 0.05 MWE /年)的加速率,从而实现了整体1986-2018期间SIACHEN MB负数( - 0.05 +/- 0.05 mWE /年)。采用不同时间尺度的SIACHEN冰川进行了少数大地测量研究的模型MB的比较(主要是2000年)。此外,模型冰川宽MB的敏感性为0.24m,0.24m,0./year,温度升高1℃,估计沉淀增加10%的敏感性为+ 0.16m. ./year。为SIACHEN GLACIER也建立了每年MB与积累面积比(AAR)和均衡线高度(ELA)的关系。

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