surface inversion

Forward modeling and inversion methods of surface wave in view of three-layer structure.

针对三层结构的面波正反演方法。

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By using the numerical Laplace inversion method, the variations of the temperature distribution along the crack surface and extended line and transient thermal stress intensity factors are presented.

利用Laplace数值反演方法，给出了裂纹面及延长线上的温度分布及动态热应力强度因子随时间变化的规律。

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Inversion of love number of earth surface by tidal strain observations

洞体应变观测资料对地表勒夫数的反演

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Coal consumption rate, topographic features, frequency of the appearance of low altitude inversion layers and frequency of surface weak winds are found to have significant effects on acid precipitation and pH value of the rain.

煤耗量、地型地貌特点、低空逆温层频率、地面弱风频率对酸雨率和降水pH值有明显的影响。

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numerical simulations with the weather research and forecasting ( wrf) model support that the cold patches cool air temperature, decelerate surface wind, and form a strong surface inversion layer up to 400m high, creating favorable conditions for sea-fog occurrence.

weather research and forecasting（WRF）模式的数值模拟表明，冷中心会降低空气的温度，形成高度达400米的表面逆温层，这些都为海雾的形成创造了有利的条件。

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During the TC, nocturnal inversion in the surface layer was enhanced through radioactive cooling along with the subsidence warming in the upper air, causing aerosol concentrations to increase at night. 5.

热带气旋影响期间，夜间地表辐射加强，加上高空的下沉增温，使得边界层逆温强度明显增大，导致夜间气溶胶浓度显著增加。

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The axes of low-layer helicity plus center is concurrent with shear line and the convergence line of surface inversion trough.

低层螺旋度大值中心轴线与切变线和地面倒槽辐合线走向一致，高层螺旋度与高空急流有关。

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This paper expounds basic method and steps of thermal infrared data inversion at gourd surface.

本文主要阐述地面热红外数据反演的基本方法和步骤。

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Waveform Inversion for Q Estimation on Walkaway VSP and Surface Seismic Data

Walkaway井地联合地震资料Q值波形反演方法

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Several Problems before inversion of surface temperatures by MODIS thermal infrared data

利用MODIS热红外数据反演地表温度前应处理的几个问题

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At first, an short introduction to the atmospheric radiation transferring model is given, then the factors impacting the aerosol optical depth inversion have been analyzed one by one, which include apparent reflectance, surface reflectance, geometry condition, atmospheric water vapor content and aerosol modes.

首先介绍了大气辐射传输模型；然后找出影响大气气溶胶反演的各个因素后逐一模拟分析，这些因子包括表观反射率、地表反射率、几何位置的变化、大气水汽含量和气溶胶模式等。

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