1) zonal propagation
纬向传播
1.
The results show that the propagations of the atmospheric ISO in the East Asian monsoon region in summer include zonal propagation and longitudinal propagation.
分析表明,夏季东亚季风区大气季节内振荡(ISO)的传播分为经向传播和纬向传播,其中经向传播主要为热带地区ISO的向北传播,纬向传播则是分别起源于印度季风区的ISO东传和起源于西太平洋海域的ISO西传。
2.
On the intraseasonal oscillation(ISO) time scale,the zonal propagation of atmospheric ISO in 2006 had its own uniqueness;the westward and stationary ISO along the latitude belt of the Yangzi River valley was weaker while the eastward and stationary ISO precipitation in Southern China.
从季节内振荡看,2006年大气季节内振荡(ISO)纬向传播与气候平均相比具有特殊性,长江流域纬度带西传波和静止波偏弱,华南地区纬度带东传波和静止波偏强,ISO这种异常与夏季长江流域降水偏少、华南降水偏多有关。
2) ISO zonal propagations
ISO纬向传播
3) back-propagation
反向传播
1.
In this paper,in order to effectively speed up the weight convergence speed of neural network,a new back-propagation algorithm is proposed.
提出了一种新的快速的误差反向传播算法 。
2.
Based on the idea of standard back-propagation(BP) learning algorithm, an improved BP learning algorithm is presented.
在标准反向传播神经网络算法的基础上,提出了一种改进的反向传播神经网络算法。
4) back propagation
反向传播
1.
Next, an Improved Back Propagation(IBP)algorithm is proposed, considering the drawbacks of the standard Back Propagation (BP) in the neural network theory.
接着,作者对神经网络理论中的标准反向传播算法BP作了改进并提出了IBP算法。
2.
Based on this framework, by making use of the back propagation method of computing partial derivatives, the maximization of mutual information can be achieved through the gradient ascent optimization process, and thus the discriminative training of HMM is performed.
基于这一框架 ,利用偏导数的反向传播计算方法 ,通过梯度上升的优化过程来实现互信息的最大化 ,从而对 HMM进行有区分力的训练 。
5) bidirectional propagation
双向传播
1.
In this study,the flood hydrograph at the forecasting section of tidal reach was considered as the superposition between flood waves from upstream and tide waves from downstream after bidirectional propagation.
将感潮河段预报断面的洪水过程视作上游洪水波和下游潮水波双向传播后的叠加,两个传播过程分别应用水位演算方法进行模拟计算,再结合多元线性回归法,以此建立同时受多个主要上游洪水及下游潮汐影响的水位预报模型。
补充资料:涂覆织物纬向拉伸强度
分子式:
CAS号:
性质:沿涂覆织物纬线方向拉伸至断裂时的最大强度。测定方法与径向拉伸强度的一样。
CAS号:
性质:沿涂覆织物纬线方向拉伸至断裂时的最大强度。测定方法与径向拉伸强度的一样。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
参考词条