1988
DOI: 10.13182/nse88-a23574
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A Time-Dependent Nodal-Integral Method for the Investigation of Bifurcation and Nonlinear Phenomena in Fluid Flow and Natural Convection

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Cited by 25 publications
(7 citation statements)
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“…Coarse-mesh nodal methods, including nodal integral methods (NIMs), have been developed over the last two decades to efficiently solve sets of linear and nonlinear PDEs [5][6][7][8][9][10][11][12]4]. Among the distinguishing features of some of the coarse mesh methods is the transverse integration process that-after the problem domain has been divided into nodes-reduces each of the PDE to an ODE by integrating over the node dimensions of all-but-one independent variables [6][7][8]10].…”
Section: Background and Motivationmentioning
confidence: 99%
“…Coarse-mesh nodal methods, including nodal integral methods (NIMs), have been developed over the last two decades to efficiently solve sets of linear and nonlinear PDEs [5][6][7][8][9][10][11][12]4]. Among the distinguishing features of some of the coarse mesh methods is the transverse integration process that-after the problem domain has been divided into nodes-reduces each of the PDE to an ODE by integrating over the node dimensions of all-but-one independent variables [6][7][8]10].…”
Section: Background and Motivationmentioning
confidence: 99%
“…Because the derivation of the TDNIM equations has been described elsewhere [7], only a brief sketch of the derivation is included here. The static nodal integral method (SNIM) equations are obtained from the TDNIM equations by forcing the time-dependent faceaveraged values to take on the node-integral-average value, and then eliminating the nodeaverage value reducing the system of 11 dynamic equations (per node) to a system of eight static equations (per node) [9].…”
Section: Summary Solution Methodsmentioning
confidence: 99%
“…NIM schemes have been developed and applied to solve fluid flow and heat transfer problems. In earlier implementations of this method, schemes were developed by clubbing the nonlinear convection terms of Navier-Stokes equations into inhomogeneous terms of ODEs generated from N-S equations [13][14][15][16]. This leads to an inefficient generation of shape functions for velocity components that captures only the diffusion process and not convection.…”
Section: Introductionmentioning
confidence: 99%
“…This leads to an inefficient generation of shape functions for velocity components that captures only the diffusion process and not convection. Moreover, use of the continuity equation to develop cell analytical solution leads to asymmetry in local solutions or shape functions of primitive variables (velocity components) in a cell [13][14][15][16]. The shortfalls of these schemes were addressed by the modified nodal integral method (MNIM) proposed by Rizwan-uddin [17].…”
Section: Introductionmentioning
confidence: 99%