Evaluation of the Equilibrium, Dynamic, and Hybrid Aerosol Modeling Approaches in a One-Dimensional Lagrangian Trajectory Model

Author(s):  
Bonyoung Koo ◽  
Spyros N. Pandis
2003 ◽  
Vol 37 (1) ◽  
pp. 53-64 ◽  
Author(s):  
Bonyoung Koo ◽  
Timothy M. Gaydos ◽  
Spyros N. Pandis

2012 ◽  
Vol 263-266 ◽  
pp. 813-816
Author(s):  
Xin Sun ◽  
Hai Jun Zhang

Established and simulated a two-dimensional amendment trajectory model for mortar. Theoretical researching and simulation show that using canard control to correct trajectory, we can change the size and direction control by adjusting the control signals. Not only can we correct one-dimensional trajectory, but also correct two-dimensional trajectory which concluding projectile range and lateral displacement, improving shooting accuracy.


Author(s):  
Kristofer Döös ◽  
Joakim Kjellsson ◽  
Bror Jönsson

1995 ◽  
Vol 07 (02) ◽  
pp. 193-242 ◽  
Author(s):  
PH.A. MARTIN ◽  
G. NENCIU

A mathematically fully controlled study of the semi-classical S-matrix associated with one-dimensional N-states systems is presented for energies above the barriers. The transmission coefficients are described by an “effective evolution” model which at high energies approaches the usual “common trajectory” model. In the two-states case a refined Landau-Zener formula describing the cross-over regime between avoided and real crossings is obtained.


2009 ◽  
Vol 3 (1) ◽  
pp. 172-186 ◽  
Author(s):  
John E. Lane ◽  
Takis Kasparis ◽  
Philip T. Metzger ◽  
W. Linwood Jones

Methodologies to improve disdrometer processing, loosely based on mathematical techniques common to the field of particle flow and fluid mechanics, are examined and tested. The inclusion of advection and vertical wind field estimates appears to produce significantly improved results in a Lagrangian hydrometeor trajectory model, in spite of very strict assumptions of noninteracting hydrometeors, constant vertical air velocity, and time independent advection during a radar scan time interval. Wind field data can be extracted from each radar elevation scan by plotting and analyzing reflectivity contours over the disdrometer site and by collecting the radar radial velocity data to obtain estimates of advection. Specific regions of disdrometer spectra (drop size versus time) often exhibit strong gravitational sorting signatures, from which estimates of vertical velocity can be extracted. These independent wind field estimates can be used as initial conditions to the Lagrangian trajectory simulation of falling hydrometeors.


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