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The Potential of GOCE in Constraining the Structure of the Crust and Lithosphere from Post-Glacial Rebound 总被引:1,自引:0,他引:1
Glacial Isostatic Adjustment (GIA) due to Pleistocene glaciation and deglaciation has left clear imprints in the present-day
geoid. The solid-earth models that are commonly used in simulating these geoid anomalies usually have the upper layer (crust/lithosphere)
elastic. While this is a good approximation for oceanic lithosphere, it is over-simplified for many continental crustal areas,
of which some are submerged at continental margins. At many places, these continental areas have a lower crustal zone that
has low viscosities. Also at the top of the mantle (asthenosphere) such zones with low viscosities can exist.
Modeling results show that, due to their shallowness and due to the laterally non-homogeneous water load, these low-viscosity
layers induce discernible signatures in the high-harmonic steady-state components of the geoid. These patchlike patterns have
typical length scales ranging from about 100 – 1000 km, and typical magnitudes of 1 cm – 1 m, depending on, a.o., depth and
width of the low-viscosity zone, viscosity and shoreline geometry.
Complications in correlating GIA modeling results with observed geoid anomalies might arise from uncertainties in isostatic
corrections (topography and non-uniform composition of crust and lithosphere) and from other non-GIA related contributions
to the observered anomalies. The characteristic forms of the patterns might assist in separating the various contributions
to the observed geoid anomalies. This can be illustrated for the Adriatic coast of Italy, where the best fit to the spatial
sea-level curve pattern is provided by a combination of GIA and regional plate tectonics.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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A.V. Kartushinsky A.Y. Sidorenko 《Advances in Space Research (includes Cospar's Information Bulletin, Space Research Today)》2013
AVHRR MCSST data for the periods 1982–2000 (mean weekly data) were used to calculate mean gradient fields in the ocean for different periods of time. Three-month averaged sea surface temperature gradients (SSTG) and their mean seasonal variations have been studied for 25 points in the large-scale oceanic fronts zones. Major oceanic fronts in the Atlantic and Pacific have been identified and compared in literature. In the North Atlantic and Pacific, the areas under study were the North Polar Front and Subpolar Fronts. In the South Atlantic and Pacific we studied the region of the Antarctic Circumpolar Current (ACC) and the fronts formed by this current, known as the South Polar Front, and the Subantarctic Front. SSTG were also calculated for El Niño (Southeast Pacific) and Benguela Current (Southeast Atlantic). 相似文献
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为系统建立可表征刚度与黏性的预浸料剥离模型,构建探针、拉伸与剥离相结合的试验验证系统。首先,设计用于预浸料的移动悬臂剥离装置,完成各工艺参数下预浸料黏性和动态刚度的90°剥离试验测定,并建立剥离仿真模型;然后,通过探针试验获取黏性参数,采用内聚力模型定量表征黏性参数;接着,通过拉伸、压缩试验测定预浸料的正交各向异性力学参数,连同探针试验获得的黏性参数一同输入到剥离模型中,在各个工艺参数下黏性和刚度的仿真结果与试验值吻合程度良好;由于仿真与试验揭示剥离脱辊现象会影响剥离力测定值,因此研究脱辊现象及其机理,发现将导辊半径设计在3~7 mm内,可减弱脱辊程度、提高剥离试验的准确性。为系统测定并表征预浸料黏性及刚度、预浸料建模、开展自动铺放仿真等提供了参考。 相似文献
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针对采用100V高压电池阵的空间站结构体带电现象,提出采用等离子体接触器进行主动电位控制方案,根据此方案建立包含接触器的空间站充放电等效电路模型,研究等离子体接触器对空间站充放电过程的影响及空间站结构因素对接触器钳位效果的影响,从而了解等离子体接触器与空间站悬浮电位的耦合特性。结果表明,无论空间站处于“快速充电”还是“正常充电”情况,等离子体接触器均能有效将空间站悬浮电位钳制在合理范围内。空间站结构因素中,电池阵暴露导体面积对接触器钳位过程影响较大,结构体暴露导体面积和结构体等效电容的影响可忽略。 相似文献
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