Abstract
Between the windward and leeward rays, boundary-layer transition on cones at angle of attack in hypersonic flow is dominated by the crossflow instability [1, 2], wherein stationary and/or traveling crossflow vortices develop and can breakdown into turbulence [3]. Stationary crossflow modes are caused by surface roughness or any other steady forcing and produce disturbances that are fixed in place on the surface [3–6]. Stationary vortices create a generalized inflection point in the velocity profile that is inviscidly unstable [7]. This distorted mean flow develops secondary instabilities, whose growth and breakdown is one path to turbulence [8–10]. Traveling crossflow modes are caused by freestream noise and/or turbulence, and cause vortical disturbances that convect with the bulk flow [3].
| Original language | American English |
|---|---|
| Journal | AIAA Journal |
| DOIs | |
| State | Published - Jan 1 2022 |
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