Moment invariants for 3D flow fields via normalization

Author(s):  
Roxana Bujack ◽  
Jens Kasten ◽  
Ingrid Hotz ◽  
Gerik Scheuermann ◽  
Eckhard Hitzer
Author(s):  
Tadd T. Truscott ◽  
Jesse Belden ◽  
Joseph R. Nielson ◽  
David J. Daily ◽  
Scott L. Thomson

Author(s):  
Jiří Dobeš ◽  
Jaroslav Fořt ◽  
Jiří Fürst ◽  
Jan Halama ◽  
Karel Kozel

2008 ◽  
Vol 3 (4) ◽  
pp. 563-575
Author(s):  
Hsien-Hsi HSIEH ◽  
Liya LI ◽  
Han-Wei SHEN ◽  
Wen-Kai TAI
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Author(s):  
Wenyao Zhang ◽  
Yuezhu Pei ◽  
Beichen Liu ◽  
Mengyuan Guan

PAMM ◽  
2012 ◽  
Vol 12 (1) ◽  
pp. 733-734 ◽  
Author(s):  
Axel Hackbarth ◽  
Edwin Kreuzer ◽  
Andrew Gray

1996 ◽  
Author(s):  
Xundong Liang ◽  
Bin Li ◽  
Shenquan Liu

2006 ◽  
Vol 9 (3) ◽  
pp. 265-274 ◽  
Author(s):  
D. H. Doh ◽  
T. G. Hwang ◽  
H. J. Jo ◽  
Y. B. Pyeon ◽  
Y. B. Cho ◽  
...  

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Eddie W. Banks ◽  
Margaret A. Shanafield ◽  
Saskia Noorduijn ◽  
James McCallum ◽  
Jörg Lewandowski ◽  
...  

2008 ◽  
Vol 47 (9) ◽  
pp. 2463-2467 ◽  
Author(s):  
Jeffrey C. Weil

Abstract A slightly simplified form of Thomson’s Lagrangian stochastic model (LSM) is presented for dispersion applications in three-dimensional (3D) flow fields. It is found that the Lagrangian velocity of a particle in 3D inhomogeneous Gaussian turbulence can be decomposed into the local Eulerian mean velocity UEi at the particle position and a velocity perturbation u′i. The Eulerian mean wind can be predicted by 3D wind field models, whereas the u′i is obtained from Thomson’s model and depends on the turbulence field. The UEi, u′i decomposition was used earlier in a two-dimensional particle model for a canopy (by Flesch and Wilson) and in models with 3D mean winds but with u′i based on LSM forms differing from that of Thomson. This note shows that the UEi, u′i decomposition is consistent with Thomson’s LSM for general 3D flow fields and is a simpler solution that should lead to improved computational efficiency for dispersion applications.


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