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Full-Stokes modeling of a polar continental glacier: the dynamic characteristics response of the XD Glacier to ice thickness

机译:全斯托克斯建模极地冰川:XD冰川到冰厚度的动态特性响应

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摘要

The steady-state diagnostic and prognostic simulation for the Xiao Dongkemadi glacier (XD) of the Tibetan Plateau was performed with the thermo-mechanically-coupled-with-Full-Stokes code Elmer (http://www.csc.fi/elmer/). In this paper, some changes of glacial thermodynamic parameters caused by ice thickness and atmospheric temperature variation were simulated in view of different thickness. The purpose of this study was to fill the gap in analyzing the ice dynamic characteristic of a polar continental glacier. The diagnostic simulation revealed the following conclusions: (1) when the thickness change was small, surface velocity, ice temperature, and deviation stress variation in the bedrock showed a tendency to change with thickness, and when the terrain was gentle, the thickness variation dominated the ice velocity. (2) The ice temperature of the bedrock was high in the whole profile and reached the pressure melting point in the terminus, and it was easy to slide at the bottom, which was consistent with the measured ground penetrating radar data near the terminus. (3) The static friction forces decrease with thickness, and they showed a complex nonlinear relationship, which revealed that the deviation stress in the bottom was influenced by thickness and ice temperature at the bedrock. The prognostic simulating from 2007 to 2047 presented: (1) The simulation forecasted a shrinkage of nearly 600 m in the terminus and the longitudinal section, and wound up diminished by nearly 25% by the end of 2047; (2) the change of thickness was small at the region between 5650 and 5700 m.a.s.l, which might be related to lower atmospheric temperature; (3) thickness dominated the deviation stress (sigma(xx) and sigma(xz)) in the bottom, and the impact of the terrain was little higher compared to deviation stress (sigma(xx)). In other words, the glacial thickness dominated the glacial force and movement to a great extent and the low temperature at high altitude reduced the XD's sensi
机译:采用热机组耦合 - 全斯托克码Elmer(http://www.csc.fi/elmer / )。在本文中,考虑到不同的厚度,模拟了由冰厚度和大气温度变化引起的冰川热力学参数的一些变化。本研究的目的是填补分析极地冰川的冰动态特性的差距。诊断仿真显示出以下结论:(1)当厚度变化小,表面速度,冰温度和基岩中的偏差应力变化显示出厚度变化的趋势,当地形温和时,厚度变化占主导地位冰速。 (2)整个型材的基岩的冰温高,达到末端的压力熔点,并且在底部易于滑动,这与终端附近的测量地面穿透雷达数据一致。 (3)静态摩擦力随着厚度而降低,并且它们显示复杂的非线性关系,这揭示了底部的偏差应力受到基岩上的厚度和冰温度的影响。从2007年到2047年的预后模拟:(1)模拟预测末端和纵向部分的近600米的收缩,并且在2047年底之前减少了近25%的伤口减少; (2)在5650至5700 m.A.1之间的区域的厚度变化小,其可能与较低的大气温度有关; (3)厚度将底部的偏差应力(Sigma(XX)和Sigma(XZ)占主导地位,与偏差应力(Sigma(XX))相比,地形的冲击略高。换句话说,冰川厚度在很大程度上占据了冰川力和运动,高海拔地区的低温降低了XD的Sensi

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  • 来源
    《Acta Mechanica》 |2018年第6期|共19页
  • 作者单位

    China Earthquake Adm Lanzhou Inst Seismol Lanzhou 730000 Gansu Peoples R China;

    Yunnan Univ Inst Int Rivers &

    Ecosecur Kunming 650091 Yunnan Peoples R China;

    Gansu Desert Control Res Inst State Key Lab Breeding Base Desertificat &

    Aeolia Lanzhou 730070 Gansu Peoples R China;

    Chinese Acad Sci Northwest Inst Ecoenvironm &

    Resources State Key Lab Cryospher Sci Lanzhou 730000 Gansu Peoples R China;

    China Earthquake Adm Lanzhou Inst Seismol Lanzhou 730000 Gansu Peoples R China;

    China Earthquake Adm Lanzhou Inst Seismol Lanzhou 730000 Gansu Peoples R China;

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  • 正文语种 eng
  • 中图分类 力学;
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