Seasonal variability of cloud optical depth over northwestern China derived from CERES/MODIS satellite measurements

The seasonal variability of cloud optical depth over northwestern China derived from Clouds and the Earth＇s Radiant Energy System （CERES） Single Scanner Footprint （SSF） Aqua Moderate Resolution Imaging Spectroradiometer （MODIS） Edition IB data from July 2002 to June 2004 is presented. The regions of interest are those with Asia monsoon influence, the Tianshan and Qilian Mountains, and the Taklimakan Desert. The results show that the instantaneous measurements presented here are much higher than the previous results derived from International Satellite Cloud Climatology Project （ISCCP） D2 monthly mean data. Generally the measurements of cloud optical depth are the highest in summer and the lowest in winter, however, Taklimakan Desert has the lowest measurements in autumn. The regional variation is quite significant over northwestern China.     

遥感可见光波段的水体透视深度研究

可见光对水体具有一定的穿透能力,有必要对其穿透深度作定量的分析评价。本文在分析前人提出的阳光穿透深度Z_(90)的基础上,综合考虑水体组成状况、大气条件和传感器接收特性等因素,提出了遥感透视深度Z_R的概念,并推导出Z_R与Z_(90)的关系式。用Landsat MSS磁带数码计算以及用Monte-Carlo法模拟低增益Landsat 3号MSS4、MSS5波段在水体含有不同悬浮泥沙和叶绿素浓度下Z_R的数值大小。结果表明,在许多情况下Z_R与Z_(90)有较大差异、     

光学介质膜在短型格兰.汤普逊棱镜中的应用

提出了一种冰洲石晶体－光学介质膜结构的短型格兰．汤普逊棱镜设计，研究了全反射光在薄膜上的透射深度，以及透射深度与棱结构角和光波长的关系。     

采面底板应力计算及应用

本文利用弹性理论推导了煤层底板任意点的应力计算公式。提出了通过计算岩石的强度指数来预计煤层底板的破坏深度。依据底板破坏深度与承压水的“原始导高”的关系预测煤层底板突水的可能性,并以现场实测数据验证了这种计算方法的可靠性。图5,表2,参考文献2。     

一种评估光学系统焦深范围的方法

本文提出绘制特征孔径的子午和弧矢场曲曲线的方法,用以控制各种象差的平衡,达到纵观光学系统焦深范围的目的。     

关于合理爆破参数的探讨

本文从以下几个方面分析了合理确定爆破参数的问题.它包括掏槽方式、炸药品种、炮孔长度,炮孔直径和爆破成本;同时给出了实用爆破参数     

Exchange Relation Planar Algebras

An inclusion of II ₁ factors NM of finite index has as an invariant, a double sequence of finite-dimensional algebras known as the standard invariant. Planar algebras were introduced by V. Jones as a geometric tool for computing standard invariants of existing subfactors as well as generating standard invariants for new subfactors. In this paper we define a class of planar algebras, termed exchange relation planar algebras, that provides a general framework for understanding several classes of known subfactor inclusions: the Fuss–Catalan algebras (i.e. those coming from the presence of intermediate subfactors) and all depth 2 subfactors. In addition, we present a new class of planar algebras (and thus a new class of subfactors) coming from automorphism subgroups of finite groups.     

起伏地表条件下的波场上延法叠前深度偏移

直接从起伏地表开始的叠前深度偏移方法是分析复杂地表和复杂地质体成像的有效手段。借鉴Beasley和Lynn提出的“零速层”的概念与Reshef提出的“逐步一累加”法的思路，根据地震波在真实介质中的传播特性及波的可叠加性，利用“波场上延”法，实现基于相移（时间域）法上延和频率空间域有限差分（深度域）法（ω-xFD）上延的波动方程法叠前深度偏移成像。理论分析和模型试算结果表明，深度域“波场上延”法是解决起伏地表和地下复杂构造双重成像的一种有效方法，实现了波动方程基准面校正和深度域成像的有机结合，其有效性和准确性使该方法可用于实际资料的处理，有较好的应用前景。