2012
DOI: 10.1007/978-94-007-2498-3
|View full text |Cite
|
Sign up to set email alerts
|

Physics of Transitional Shear Flows

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
12
0
9

Year Published

2012
2012
2023
2023

Publication Types

Select...
5
4
1

Relationship

0
10

Authors

Journals

citations
Cited by 55 publications
(21 citation statements)
references
References 93 publications
0
12
0
9
Order By: Relevance
“…The simplest one consists in transforming it to a linear problem of larger dimension by forming the so-called companion matrices [20]. A companion matrix for equation (42) …”
Section: ( ))mentioning
confidence: 99%
“…The simplest one consists in transforming it to a linear problem of larger dimension by forming the so-called companion matrices [20]. A companion matrix for equation (42) …”
Section: ( ))mentioning
confidence: 99%
“…It is thus suggested that a hairpin-regeneration cycle exists at each local scale, until the limiting scales defined by viscous dissipation. This scenario of transition accounts for the preponderance of hairpin structures in transitional boundary layers, as observed in both experiments (Boiko et al 2012) and numerical studies (Wu and Moin 2009).…”
Section: Resultsmentioning
confidence: 52%
“…Moreover, if A and E are Hermitian and A is positive or negative definite, then ν = µ, P l = P For example in the interconnect analysis of VLIC [5] and the linear stability analysis of hydrodynamic flows [2]. Without loss of generality we will assume that the matrix A is nonsingular since otherwise the change of variable x =xe ρt , where ρ is chosen such that A − ρE is nonsingular, leads to a system forx of the same form as (4.1) but with a nonsingular matrix A − ρE instead of A.…”
Section: Letmentioning
confidence: 99%