Non-orthogonal plane-marching parabolized stability equations for the secondary instability of crossflow vortices

Journal Article (2026)
Author(s)

K.J. Groot (TU Delft - Aerodynamics, University of Wyoming)

J. Casacuberta Puig (TU Delft - Aerodynamics)

S. Hickel (TU Delft - Aerodynamics)

Research Group
Aerodynamics
DOI related publication
https://doi.org/10.1016/j.compfluid.2025.106947
More Info
expand_more
Publication Year
2026
Language
English
Research Group
Aerodynamics
Bibliographical Note
Green Open Access added to TU Delft Institutional Repository as part of the Taverne amendment. More information about this copyright law amendment can be found at https://www.openaccess.nl. Otherwise as indicated in the copyright section: the publisher is the copyright holder of this work and the author uses the Dutch legislation to make this work public.@en
Volume number
306
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

A detailed derivation, analysis, and verification is given for the non-orthogonal, plane-marching Parabolized Stability Equations (PSE) approach. In applying the approach to a flow distorted by a medium-amplitude crossflow vortex, we determine its linear secondary instability mechanisms. We show that converged solutions can be achieved for a broad frequency range with an existing stabilization method for the line-marching PSE approach. We verify that 1) solutions converge versus grid size in all dimensions, 2) primary disturbance solutions agree with line-marching PSE results, and 3) secondary disturbance solutions match amplitude and growth-rate evolution of reference Direct Numerical Simulation (DNS) results. We show how and why the type-II instability displays a delayed neutral point when modeled with the plane-marching approach versus the considered local stability approaches, whether the streamwise evolution of the distorted base flow is accounted for or not. This may explain why the type-II disturbance is scarcely captured by DNS in the literature.

Files

License info not available
warning

File under embargo until 17-06-2026