一类三物种竞争-互助型反应扩散方程解的渐近行为

研究了一般类型的三个物种之间竞争一互助型反应扩散方程解的渐近行为，并且给出了该类型反应扩散系统一种新的单调迭代格式．主要利用上、下解方法和特征值理论，通过对原方程的线性微分算子的谱加以限定，得到了系统的全局吸引子和该系统在某些条件下三物种能够相互共存，而在另一些务件下有物种趋向灭绝的结论．     

无界槽形区域上Boussinesq方程的整体吸引子

该文讨论了无界域上Boussinesq方程解的渐近行为，证明了在一定条件下，Boussinesq方程整体吸引子的存在笥及其整体吸引子具有有限的Hausdorff维数。作者将主要利用加权Sobolev空间的估计技巧讨论无界域上吸收集的紧性。     

A piecewise-integration method for simulating the influence of external forcing on climate

Climate drift occurs in most general circulation models （GCMs） as a result of incomplete physical and numerical representation of the complex climate system, which may cause large uncertainty in sensitivity experiments evaluating climate response to changes in external forcing. To solve this problem, we propose a piecewise-integration method to reduce the systematic error in climate sensitivity studies. The observations are firstly assimilated into a numerical model by using the dynamic relaxation technique to relax to the current state of atmosphere, and then the assimilated fields are continuously used to reinitialize the simulation to reduce the error of climate simulation. When the numerical model is integrated with changed external forcing, the results can be split into two parts, background and pertur- bation fields, and the background is the state before the external forcing is changed. The piecewise-integration method is used to con- tinuously reinitialize the model with the assimilated field, instead of the background. Therefore, the simulation error of the model with the external forcing can be reduced. In this way, the accuracy of climate sensitivity experiments is greatly improved. Tests with a simple low-order spectral model show that this approach can significantly reduce the uncertainty of climate sensitivity experiments.     

Neumann边条件无电容效应Sine-Gordon系统的动力学

证明当扩散系数适当大时Neumann边条件下无电容效应的Sine Gordon系统全局吸引子是一条不变曲线 ,系统在其上的行为类似于圆周上的保向同胚 .     

一类反应扩散方程组的拟解与全局吸引子

目的研究一类具有齐次Dirichlet边界条件的抛物系统的全局吸引子及其对应的平衡态系统的拟解,该问题产生于生态学中三物种捕食-食饵模型。方法采用上下解的方法、单调迭代法、比较原理、极值原理以及特征值理论进行了研究。结果得到了这类捕食-食饵模型平衡态系统的拟解。结论对任意非平凡非负初值,上述三物种模型具有全局吸引子。     

含参Sprott-O混沌系统的直接延迟反馈控制

利用非线性动力学理论,讨论了带有参数的Sprott-O系统的混沌特性.利用数值方法得到系统的混沌吸引子和周期态.在(2.65,2.95)区间内,运用全局分岔图和Lyapunov指数图准确地表征了系统在此区间内丰富的非线性行为.通过局部放大的全局分岔图,发现系统发生了倒倍周期分岔现象.最后应用直接延迟反馈法对系统的混沌运动进行了控制,使系统的混沌运动控制到稳定的低周期运动状态.     

加法噪声驱动的随机Lorenz系统吸引子及其上半连续性

确定的Lorenz系统是描述大气运动规律的重要数学模型,具有深厚的应用背景,被许多学者广泛研究,然而气候环境受突变因素影响,确定的情形无法完全解释大气的运动规律性;基于此,研究了一种基于加法白噪声驱动的随机Lorenz系统的渐进行为,通过恰当的估计证明了系统在参数不受约束条件下存在随机吸收集,进而获得了随机Lorenz...     

弱耗散的广义 Camassa-Holm 方程整体吸引子

在一定边界条件下研究一类新的带弱耗散项的色散水波方程的动力学行为,获得其整体解及整体吸引子的存在.     

Sprott-F系统的混沌控制研究

利用非线性动力学理论,讨论了改进的Sprott-F系统的混沌特性.在参数区b E[0,0.5]上,利用全局分岔图,Lyapunov指数谱准确的表征了系统在此区间内的丰富的非线性行为.应用时滞反馈法、比例微分器控制法和x|x|法对系统的混沌控制进行了详尽全面的理论分析和数值模拟.结果表明,选择适当的反馈系数,通过以上三种控制法,可将系统的混沌运动控制到稳定的低周期状态.     

广义Newton-Boussinesq方程组的整体吸引子(英文)

研究Newton-Boussinesq方程组解的长时间行为. 通过一致先验估计,证明了周期边值问题整体吸引子的存在性,得到了整体吸引子Hausdorff维数及分形维数的上界估计.     

三模Lorenz系统的动力学行为及其数值仿真

考虑三模Lorenz系统的动力学行为及其数值模拟,证明了该方程组吸引子的存在性,并分析讨论了其全局稳定性,数值模拟了参数在一定范围内变化时,三模Lorenz系统混沌的发生过程.     

时滞反馈法控制含3参数的Sprott N混沌系统

利用非线性动力学理论,讨论了含有3个参数的Sprott N系统的混沌特性.在参数区间b∈[1.8,2.5]上,利用全局分岔图,Lyapunov指数谱准确的表征了系统在此区间内的丰富的非线性行为.应用时滞反馈法对系统的混沌控制进行了详细的理论分析和数值模拟.结果表明,通过该控制法,可将系统的混沌运动控制到稳定的周期运动状态.     

一类S 分布时滞递归神经网络的全局吸引子

研究了一类S 分布时滞递归神经网络的渐近行为,通过构造一类带有Razuminkhin条件的Lyapunov函数,证明了系统的耗散性。利用算子分解的方法讨论了网络模型的渐近紧性,结合吸引子的理论给出了全局吸引子存在的充分条件。     

一类时滞微分方程的全局吸引子的存在性

对于在实际中经常出现的一类时滞微分方程dx(t)/dt=f(x(t),x(t-1))，给出了其全局吸引子的存在的条件，推广了有关的结论。     

带逆平方势的非线性Shroedinger方程整体吸引子及其维数估计

研究了带逆平方势的非线性Shroedinger方程的长时间动力学行为，证明了整体吸引子的存在性，并给出了整体吸引子的Hausdorff维数和Fractal维数的上界估计．     

含时滞的耦合Fitz-Hugh-Nagumo系统的全局吸引子

文章讨论了含时滞的耦合Fitz-Hugh-Nagumo(FHN)反应扩散系统的长时间行为。由于时滞项的出现。将造成解的先验估计的困难。为此通过构造一个合适的Lyapunov泛函。给出了时滞的耦合FHN系统的全局吸引子存在的一个充分条件。     

Impacts of external forcing on the 20th century global warming

The impacts of external forcing,including natural and anthropogenic,on the 20th century global warming were assessed with the use of the Grid Atmospheric Model of IAP/LASG Version 1.1.0,fol-lowing the standard coordinated experiment design of the Climate Variability and Predictability(CLIVAR) International Climate of the Twentieth Century Project(C20C) ,Phase II. The results indicate that external forcing plays an important role in the evolution of the land surface air temperature on in-terannual,decadal,and interdecadal time scales,and contributes greatly to the global warming in the following two periods:the early twentieth century between the 1910s and the 1940s and the late twen-tieth century after the 1970s. External forcing also has strong impact on the regional temperature change during the two warming periods except for parts of the Eurasia and the North America conti-nents. In the cooling period,however,the impact of internal variability is dominant.     

Climate sensitivity constrained by temperature reconstructions over the past seven centuries

The magnitude and impact of future global warming depends on the sensitivity of the climate system to changes in greenhouse gas concentrations. The commonly accepted range for the equilibrium global mean temperature change in response to a doubling of the atmospheric carbon dioxide concentration, termed climate sensitivity, is 1.5-4.5 K (ref. 2). A number of observational studies, however, find a substantial probability of significantly higher sensitivities, yielding upper limits on climate sensitivity of 7.7 K to above 9 K (refs 3-8). Here we demonstrate that such observational estimates of climate sensitivity can be tightened if reconstructions of Northern Hemisphere temperature over the past several centuries are considered. We use large-ensemble energy balance modelling and simulate the temperature response to past solar, volcanic and greenhouse gas forcing to determine which climate sensitivities yield simulations that are in agreement with proxy reconstructions. After accounting for the uncertainty in reconstructions and estimates of past external forcing, we find an independent estimate of climate sensitivity that is very similar to those from instrumental data. If the latter are combined with the result from all proxy reconstructions, then the 5-95 per cent range shrinks to 1.5-6.2 K, thus substantially reducing the probability of very high climate sensitivity.     

狄氏边条件无电容效应的Sine-Gordon系统的动力学

证明无电容效应的Sine Gordon系数的全局吸引子的存在性 ,并指出当扩散系统适当大时全局吸引子即为系统的唯一周期解 .还证明系统在自治情形时是一个梯度系统 .     

非经典扩散方程的时间依赖强全局吸引子的存在性

本文在具有光滑边界的有界域上考虑了非经典扩散方程并在强拓扑空间中讨论了该问题解的长时间行为. 所用方法基于Meng和Liu引入并且证明的时间依赖全局吸引子存在性的充分条件.