Finite commutative group; Symmetric bicharacter; Lie color superalgebra ; Left color symmetric algebra ; Left color symmetric structure

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The conditional symmetry instability is the intermediate process between the stable and instable states of the atmosphere. The evolution of the atmosphere from the stable to unstable state or from unstable to stable state comes through two stages. The convective-symmetric instability circulation is related with the state and type of the instability. When the conditional instability lies in the lower level and conditional symmetric instability in the upper level, the circulation will have vertical updrafts in the lower level and slantwise updrafts in the upper level. The release of conditional symmetric instability gives rise to a mesoscale rain belt.

結(jié)果表明：條件對(duì)稱不穩(wěn)定是大氣穩(wěn)定狀態(tài)和條件不穩(wěn)定狀態(tài)之間的中間紐帶女人16一毛片，大氣由穩(wěn)定向不穩(wěn)定或者由不穩(wěn)定向穩(wěn)定的演變均通過條件對(duì)稱不穩(wěn)定來實(shí)現(xiàn)；對(duì)流對(duì)稱不穩(wěn)定環(huán)流的形成與不穩(wěn)定層的配置有關(guān)日本性爱三级片免费在线播放，當(dāng)?shù)蛯訛闂l件不穩(wěn)定而高層疊加深厚的條件對(duì)稱不穩(wěn)定時(shí)国产平胸美女在线观看，對(duì)流對(duì)稱不穩(wěn)定環(huán)流低層出現(xiàn)垂直上升氣流，高層出現(xiàn)范圍較廣的傾斜上升氣流五月社社社色区，對(duì)稱不穩(wěn)定能量釋放產(chǎn)生中尺度云帶40分钟视频在线观看免费黄。

The conclusion of this article contains:(1) The climatology symmetric index and antisymmetric index which represent the uniform system of ocean and atmosphere is defined according to the unique kinetic character of the large-scale fluid. The symmetric mode, a state mode, and antisymmetric mode, a propagate westward mode, of ocean and atmosphere are distinguished clearly from each other. Also, the primary part which determines the symmetric mode emerges from non-divergenct wind and the dominant part which contributes to the antisymmetric mode mostly is irrotational wind. The article also compares the disparity of the climatology distribution of SST and sea surface wind field between 1948-1975 and 1976-2005. The SST of both the tropical Indian Ocean and the tropical Pacific after 80's is warm than before 80's .

主要結(jié)論如下：(1)熱帶太平洋氣候平均態(tài)所包含的海-氣相互作用的資料分析根據(jù)海洋和大氣的運(yùn)動(dòng)特性，定義了表征海洋大氣系統(tǒng)的對(duì)稱模態(tài)和反對(duì)稱模態(tài)指數(shù)欧美日本大片在线观看黄，通過兩個(gè)指數(shù)對(duì)熱帶太平洋和印度洋關(guān)于赤道對(duì)稱和反對(duì)稱的兩個(gè)模態(tài)進(jìn)行區(qū)分久久A毛片超清无码一区二区三区，發(fā)現(xiàn)關(guān)于赤道反對(duì)稱的海-氣耦合模態(tài)主要包含了大氣散度分量和海洋SST的相互作用；關(guān)于赤道對(duì)稱的海-氣耦合模態(tài)主要包含了大氣旋度分量和海洋SST的相互作用A级黄丝袜网站，并從資料估算了該耦合模態(tài)向西傳播的速度国产精品湿润。

This thesis mainly discuss following issues, Theory and simple expressions for array covariance matrixes are derived when angular spread functions are symmetric distribution functions, i. e. the Uniform distribution, the Gauss distribution, the Laplace distribution and the Von Mises distribution, and a non-symmetric distribution function, i. e. the Gamma distribution. And the relation between the effective signal subspace and the array number, or and the nominal angle of the distributed source, the angular spread, the distributed functions, and the Signal-to-Noise Ratio is gained. The dimension of the effective signal subspace increases with increment of the array number. And it is more obvious to the non-symmetric distribution. The dimension of the effective signal subspace decreases with increment of the nominal angle. And the distributed source is equal to a point source as θ=π/2. The dimension of the effective signal subspace increases with increment of the angular spread.

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The solution group such as symmetric, skew-symmetric, centrosymmetric, centroskew symmetric, reflexive, antireflexive, bisymmetric or symmetric and antipersymmetric are successfully found.

構(gòu)造了一種迭代法系統(tǒng)地研究了問題Ⅴ的一般解組、對(duì)稱解組91精品有码在线、中心對(duì)稱解組欧美色图亚洲图区、自反矩陣解組、雙對(duì)稱解組超碰在线视屏观看、對(duì)稱次反對(duì)稱解組及其最佳逼近等問題www.MADOUav.com，并成功地解決了這些問題。

Non-symmetric kernel density estimation is first used for life-table graduation in order to solve boundary bais of symmetric kernel used in the standard kernel density estimator,and compare the symmetric kernel graduation with non-symmetric kernel graduation and obtain the satisfied result.

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In this paper we separate the Hamiltonian into three parts: a spherical symmetry Hamiltonian; a z-component of the angular momentum operator, and a non-spherical symmetric potential as the perturbation operator, and provide a propose method by separating the potential containing squared magnetic field B^2 into two parts spherical symmetric and non-spherical symmetric ones so that the first-order energy correction due to the non-spherical symmetric potential is zero, and the second-order correction due to B^2 can be obtained by a simple variational method.

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In many practice problems such as to know the resonnance frequency of a structure and to know the critical value for the stability of a dynamical system,often need to compute the eigenvalues of a symmetric matrix. The chief method to compute the eigenvalues of a symmetric matrix is first to transformate the matrix to a symmetric tridiagonal matrix similarly and orthogonally, then to use the QR method with shift to the symmetric tridiagonal matrix.

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Problem III Given find such thatProblem IV When Problem I or II or III is consistent, let Se denote the set of its solutions, for given , find , such thatwhere is Frobenius norm, S is Rn×p or a subset of Rn×p satisfying some constraint conditions, such as symmetric, skew-symmetric, centrosymmet-ric, centroskew symmetric, reflexive, antireflexive, bisymmetric or symmetric and antipersymmetric.

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R~, find∈S_E, such that ProblemⅤGiven, find [X_1,X_2,…,X_l](where X_i∈S_i,i=1,2,…,l), such that A_1X_1B_1+A_2X_2B_2+…+A_lX_lB_l=C ProblemⅥWhen ProblemⅤis consistent, let SE denote the set of its solutions, for given,find, such that where||·|| is Frobenius norm, S and S_i are the matrix set satisfying some constraint conditions such as symmetric, skew-symmetric, centrosymmetric, centroskew symmetric, reflexive, antireflexive, bisymmetric or symmetric and antipersymmetric.

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