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Peter A. Monkewitz

Researcher at École Polytechnique Fédérale de Lausanne

Publications -  110
Citations -  9004

Peter A. Monkewitz is an academic researcher from École Polytechnique Fédérale de Lausanne. The author has contributed to research in topics: Reynolds number & Turbulence. The author has an hindex of 37, co-authored 107 publications receiving 8393 citations. Previous affiliations of Peter A. Monkewitz include University of California & University of California, Los Angeles.

Papers
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Local and global instabilities in spatially developing flows

TL;DR: In this article, a review of recent developments in the hydro- dynamic stability theory of spatially developing flows pertaining to absolute/convective and local/global instability concepts is presented.
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Absolute and convective instabilities in free shear layers

TL;DR: The absolute or convective character of inviscid instabilities in parallel shear flows can be determined by examining the branch-point singularities of the dispersion relation for complex frequencies and wavenumbers.
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Wall-bounded turbulent flows at high Reynolds numbers: Recent advances and key issues

TL;DR: In this paper, the authors distill the salient advances of recent origin, particularly those that challenge textbook orthodoxy, and highlight some of the outstanding questions, such as the extent of the logarithmic overlap layer, the universality or otherwise of the principal model parameters, and the scaling of mean flow and Reynolds stresses.
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The need for a pressure-term representation in empirical Galerkin models of incompressible shear flows

TL;DR: In this paper, a low-dimensional empirical Galerkin model is developed for spatially evolving laminar and transitional shear layers, based on a Karhunen-Loeve decomposition of incompressible two-and three-dimensional Navier-Stokes simulations.
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Influence of the velocity ratio on the spatial instability of mixing layers

TL;DR: In this article, the linear spatial instability of the tanh and Blasius mixing layers is studied for different values of the ratio between the difference and the sum of the velocities of the two co-flowing streams.