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The author introduces process, designs, models, hypotheses, and estimated variance component of Generalizability Theory at length on the basis of three kinds of educational test theories.

本文在简要回顾三大测量理论的基础上,较详细的阐述了概化理论的步骤、设计方案、模型和假设、方差分量估计等。

Secondly, the combination in concept and problem teaching can enhance profound comprehension of Exclusive Events and Independent Events. Finally, because Distribution is basic knowledge in teaching probability, meanwhile, the calculation for Expected Value and Variance also are based on Distribution. Thus, Distribution is the most important in teaching them, it needs to give more emphasis.

其中计算机模拟手段在概率的频率定义教学中效果明显,并且直观模型在古典概型教学中的作用也相当明显;其次,通过概念教学与解题教学的结合可以帮助学生深刻理解互斥事件与独立事件;最后,随机变量的分布列作为概率基础知识,期望以及方差的计算都是以分布列为基础的,因而,强化分布列的教学是这部分内容的重中之重。

But he also figured that the concept of "range probable error" would work in his favor.

但是维斯中尉还是指望着炮兵技术概念里的"射程概差"能给他带来运气。

The equations of optimal probability density function of stochastic variable or limit state function are derived by use of the higher moments of the function.

一次二阶矩法主要利用随机变量的均值和方差信息以及分布概型来计算结构的失效概率,属于低阶矩法。

The results show that with the sea level rise, amphidromic point in this sea area tends to move to the southeast, and then coastal tidal ranges change present consequently different features ,that is,at the left side and bayhead coast near the amphidromic point they change evidently, and little at the right side and bayhead coast far away from amphidromic point.

将南黄海概化为一等深矩形海域,初步研究了在海平面上升3m 和 5m 条件下该海域旋转潮波系统的演化趋势,继而分析了沿岸潮差变化特征。初步分析研究表明:随着海平面上升,该海域 M2 分潮的无潮点有向东南方向偏移的趋势,受此影响,沿岸潮差呈现不同的变化特征,靠近无潮点的左侧及湾顶海岸变化明显,而远离无潮点的右侧及湾顶海岸则变化不大。

The results show that with the sea level rise, amphidromic point in this sea area tends to move to the southeast, and then coastal tidal ranges change present consequently different features ,that is,at the left side and bayhead coast near the amphidromic point they change evidently, and little at the right side and bayhead coast far away from amphidromic point.

将南黄海概化为一等深矩形海疆,初阶研究了在海平面上升3m 和 5m 前提下该海疆扭转潮波体系的演化趋势,继而剖析了沿岸潮差厘革特性。初阶分析研究剖明:跟着海平面上升,该海疆 M2 分潮的无潮点有向东南标的目的偏移的趋势,受此影响,沿岸潮差泛起差此外厘革特性,接近无潮点的左侧及湾顶海岸厘革较着,而阔别无潮点的右侧及湾顶海岸则厘革不年夜。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域,初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势,继而分析了沿岸潮差变化特征。初应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域,初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势,继而分析了沿岸潮差变化特征。初步分析研;应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海疆,初阶研究了在海平面上升 3m 和 5m 前提下该海疆扭转潮波体系的演化趋势,继而剖析了沿岸潮差厘革特应用海湾和半封闭矩形海疆改造的 Taylor 题目的解研究海平面上升对 M2 分潮扭转潮波体系及沿岸潮差的厘革。

Schematizing the southern Yellow sea as an constant water depth and semi-enclosed rectangular bay, the evolution trends of tidal amphidromic system of M2and variation features of coast tidal range are analyzed primary under the condition of 3 and 5 meter rise of sea level respectively.

将南黄海概化为一等深矩形海域,初步研究了在海平面上升 3m 和 5m 条件下该海域旋转潮波系统的演化趋势,继而分析了沿岸潮差变化特征。初步分析研究表明:随着海平面上升,该海域 M2 分潮的无潮点有向东南方向偏移的趋势,受此影响,沿。。。应用海湾和半封闭矩形海域改进的 Taylor 问题的解研究海平面上升对 M2 分潮旋转潮波系统及沿岸潮差的变化。

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Plunder melds and run with this jewel!

掠夺melds和运行与此宝石!

My dream is to be a crazy growing tree and extend at the edge between the city and the forest.

此刻,也许正是在通往天国的路上,我体验着这白色的晕旋。

When you click Save, you save the file to the host′s hard disk or server, not to your own machine.

单击"保存"会将文件保存到主持人的硬盘或服务器上,而不是您自己的计算机上。