| 大地测量观测和相对海平面联合约束的冰川均衡调整模型 |
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| 引用本文： | 汪汉胜,WU Patrick,贾路路,胡波,王志勇.大地测量观测和相对海平面联合约束的冰川均衡调整模型[J].地球物理学报,2009,52(10):2450-2460. |
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| 作者姓名： | 汪汉胜 WU Patrick 贾路路 胡波 王志勇 |
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| 作者单位： | 1.中国科学院测量与地球物理研究所动力大地测量学重点实验室，武汉 430077;2.Department of Geoscience, University of Calgary, Alberta, Canada T2N 1N4;3.Department of Earth Observation and Space Systems, Delft University of Technology, Delft, The Netherlands, 2629 HS;4.中国科学院研究生院，北京 100049;5.山东理工大学建工学院，淄博 255049 |
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| 基金项目： | 国家杰出青年科学基金(40825012) |
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| 摘 要： | 利用大地测量和历史相对海平面变化数据，结合地震剪切波层析模型，联合确定了新的末次冰期冰川均衡调整（GIA）模型，其中地幔黏滞度不仅沿径向而且沿横向变化.研究思路是，先尝试性地选择比例系数β，利用与地震剪切波速异常的线性关系，计算地幔黏滞度横向扰动，并与横向均匀的黏滞度参考模型叠加给出3D地幔黏滞度模型；再利用耦合拉普拉斯方程的有限元法算法进行GIA预测；然后，重复该过程，直到预测与观测之间的吻合满意为止.主要结论有：（1）给出了横向非均匀的地幔黏滞度模型（RF3L20(β=0.4)），发现了黏滞度显著的横向非均匀性和其对GIA预测的显著影响，指出横向非均匀不完全是由热效应引起的，可能还与化学组分等其他因素有关，该模型可用于地幔动力学研究.（2）给出了全球现今多种GIA预测速率，可为板块运动、陆地水储量、海水质量变化和冰川冰雪质量非平衡监测提供重要的改正.
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| 关 键 词： | 大地测量观测 相对海平面 冰川均衡调整 横向非均匀 地幔黏滞度 |
| 收稿时间： | 2009-8-4 |
| 修稿时间： | 2009-9-21 |
Glacial isostatic adjustment model constrained by geodetic measurements and relative sea level |
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| WANG Han-Sheng,WU Patrick,van der Wal Wouter,JIA Lu-Lu,HU Bo,WANG Zhi-Yong.Glacial isostatic adjustment model constrained by geodetic measurements and relative sea level[J].Chinese Journal of Geophysics,2009,52(10):2450-2460. |
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| Authors: | WANG Han-Sheng WU Patrick van der Wal Wouter JIA Lu-Lu HU Bo WANG Zhi-Yong |
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| Institution: | 1.Key Laboratory of Dynamical Geodesy, Institute of Geodesy & Geophysics, Chinese Academy of Sciences, Wuhan 430077, China;2.Department of Geoscience, University of Calgary, Calgary T2N 1N4, Canada;3.Department of Geomatics Engineering, University of Calgary, Alberta, Canada T2N 1N4;4.Graduate Universty of Chinese Academy of Sciences, Beijing 100049, China;5.School of Architecture Engineering, Shandong University of Tecnology, Zibo 255049, China |
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| Abstract: | The new model of the last glacial isostatic adjustment (GIA) is constrained simutaneously by the data sets from geodetic measurements, relative sea levels and seismic shear tomographic data. The viscosities in mantle for this model are allowed to vary both radially and laterally. Firstly, the scalling factor β is tentatively chosen for which the lateral perturbations in viscosity are computed based on the linear relation with seismic shear wave anomalies. These lateral perturbations in viscosity are then supperposed logarithmically on a laterally homogeneous reference viscosity model to give the total viscosities in the mantle layers. Based on this 3-D viscosity model, the GIA predictions are computed using the coupled-Laplace Finite-Element Method. Such processes will not end untill the predictions agree well with the observed data sets. The main results are as follows. Firstly, the laterally heterogeneous viscosity model (RF3L20(β =0. 4)) is determined from which the obvious lateral heterogeneities and the prominouced effects on GIA predictions are found. It is indicated the lateral heterogeneities are attributable not just to themal effects but also to lateral variations in chemistry and other factors. The RF3L20(β = 0. 4) model can be used to the modelling in mantle geodynamics. Secondly, the multiple present GIA rates are predicted that can be served as the important corrections for the monitoring of the tectonic motion, land water storage changes, ocean water mass variations and the non-equilibrium of the ice and snow. |
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| Keywords: | Geodetic measurements Relative sea level Glacial isostatic adjustment Lateral heterogeneity Mantle viscosity |
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