M
Monisha Roy
Researcher at Indian Institute of Technology Madras
Publications - 18
Citations - 429
Monisha Roy is an academic researcher from Indian Institute of Technology Madras. The author has contributed to research in topics: Combined forced and natural convection & Heat transfer. The author has an hindex of 10, co-authored 18 publications receiving 323 citations. Previous affiliations of Monisha Roy include Karnatak University.
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Studies on natural convection within enclosures of various (non-square) shapes – A review
TL;DR: In this paper, a review of the studies on natural convection heat transfer in triangular, trapezoidal, parallelogrammic enclosures and enclosures with curved and wavy walls filled with fluid or porous media is presented.
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Role of various moving walls on energy transfer rates via heat flow visualization during mixed convection in square cavities
Monisha Roy,S. Roy,Tanmay Basak +2 more
TL;DR: In this paper, the authors analyzed the heat flow distribution in closed cavities with different types of walls, including isothermally hot bottom wall, cold side walls and insulated top wall.
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Triple diffusive mixed convection along a vertically moving surface
TL;DR: In this paper, a numerical investigation on steady triple diffusive mixed convection boundary layer flow past a vertical plate moving parallel to the free stream in the upward direction is presented, where sodium chloride and Sucrose are chosen as solutal components which are added in the flow stream from below with various concentration levels.
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Analysis of Entropy Generation for Mixed Convection in a Square Cavity for Various Thermal Boundary Conditions
TL;DR: In this paper, finite element simulations were carried out to analyze entropy generation during mixed convection inside square enclosures with an isothermally hot bottom wall, adiabatic top wall, and linearly heated side walls.
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Role of the importance of ‘Forchheimer term’ for visualization of natural convection in porous enclosures of various shapes
TL;DR: In this paper, the importance of the quadratic (Forchheimer) drag force for the flow through porous media during natural convection within various geometrical shapes (square, rhombus, concave and convex).