论文标题
部分可观测时空混沌系统的无模型预测
Rotational Dependence of Large-scale Dynamo in Strongly-stratified Convection: What Causes It?
论文作者
论文摘要
储层计算是预测湍流的有力工具,其简单的架构具有处理大型系统的计算效率。然而,其实现通常需要完整的状态向量测量和系统非线性知识。我们使用非线性投影函数将系统测量扩展到高维空间,然后将其输入到储层中以获得预测。我们展示了这种储层计算网络在时空混沌系统上的应用,该系统模拟了湍流的若干特征。我们表明,使用径向基函数作为非线性投影器,即使只有部分观测并且不知道控制方程,也能稳健地捕捉复杂的系统非线性。最后,我们表明,当测量稀疏、不完整且带有噪声,甚至控制方程变得不准确时,我们的网络仍然可以产生相当准确的预测,从而为实际湍流系统的无模型预测铺平了道路。
In a rigidly-rotating magnetohydrodynamic (MHD) system with convective turbulence, a large-scale dynamo, categorized as the $α^2$-type, can be excited when the spin rate is large enough. In this paper, the rotational dependence of the $α^2$-type dynamo and the cause of it are explored by mean-field (MF) dynamo models coupled with direct numerical simulations (DNSs) of MHD convections. Bearing the application to the solar/stellar dynamo in mind, we adopt a strongly-stratified polytrope as a model of the convective atmosphere. Our DNS models show that the $α^2$-type dynamo is excited when ${\rm Ro} \lesssim 0.1$ where ${\rm Ro}$ is the Rossby number defined with the volume-averaged mean convective velocity. From the corresponding MF models, we demonstrate that the rotational dependence of the $α^2$-type dynamo is mainly due to the change in the magnitude of the turbulent magnetic diffusion. With increasing the spin rate, the turbulent magnetic diffusion weakens while the $α$-effect remains essentially unchanged over the convection zone, providing the critical point for the excitation of the large-scale dynamo. The ${\rm Ro}$-dependence of the stellar magnetic activity observable in the cool star is also discussed from the viewpoint of the rotational dependence of the turbulent electro-motive force. Overall our results suggest that, to get a better grasp of the stellar dynamo activity and its ${\rm Ro}$-dependence, it should be quantified how the convection velocity changes with the stellar spin rate with taking account of the rotational quenching and the Lorentz force feedback from the magnetic field on the convective turbulence.