On the stability of Maxwell distribution for a system of thermals in turbulent convective layers of fresh and salt water bodies
- Authors: Vul’fson A.N.1, Borodin O.O.1
- 
							Affiliations: 
							- Oil and Gas Research Institute
 
- Issue: Vol 43, No 1 (2016)
- Pages: 66-72
- Section: Hydrophysical Processes
- URL: https://journals.rcsi.science/0097-8078/article/view/173794
- DOI: https://doi.org/10.1134/S0097807816010152
- ID: 173794
Cite item
Abstract
An ensemble of cold thermals in a convective layer of a fresh or salt water body is considered. The probability distribution density of the vertical velocities of thermals is assumed to satisfy the K-form of Fokker−Planck equation. The K-form of the Fokker−Planck equation is shown to have a steady-state solution in the form of a generalized Maxwell distribution. Natural and numerical experiments were carried out to demonstrate the existence of such distribution. Lyapunov functional in the form of Kullback relationship was used to establish the nonlinear instability of this distribution with respect to small perturbations in the Hilbert space norm.
About the authors
A. N. Vul’fson
Oil and Gas Research Institute
							Author for correspondence.
							Email: vulfson@ipng.ru
				                					                																			                												                	Russian Federation, 							ul. Gubkina 3, Moscow, 109333						
O. O. Borodin
Oil and Gas Research Institute
														Email: vulfson@ipng.ru
				                					                																			                												                	Russian Federation, 							ul. Gubkina 3, Moscow, 109333						
Supplementary files
 
				
			 
					 
						 
						 
						 
						 
				 
  
  
  
  
  Email this article
			Email this article  Open Access
		                                Open Access Access granted
						Access granted Subscription Access
		                                		                                        Subscription Access
		                                					