Cumulative reaction probability via transition state wave packets

1996 ◽  
Vol 104 (16) ◽  
pp. 6184-6191 ◽  
Author(s):  
Dong H. Zhang ◽  
John C. Light
Keyword(s):  
Transition State ◽  
Wave Packets ◽  
Reaction Probability ◽  
State Wave

Well converged quantum rate constants for the H2+ OH → H2O + H reaction via transition state wave packet

2018 ◽  
Vol 149 (6) ◽  
pp. 064303 ◽  
Author(s):  
Peng Sun ◽  
Zhaojun Zhang ◽  
Jun Chen ◽  
Shu Liu ◽  
Dong H. Zhang
Keyword(s):  
Wave Packet ◽  
Transition State ◽  
Rate Constants ◽  
State Wave

Cumulative isomerization probability studied by various transition state wave packet methods including the MCTDH algorithm. Benchmark: HCN→CNH isomerization

2004 ◽  
Vol 121 (2) ◽  
pp. 644-654 ◽  
Author(s):  
B. Lasorne ◽  
F. Gatti ◽  
E. Baloitcha ◽  
H.-D. Meyer ◽  
M. Desouter-Lecomte
Keyword(s):  
Wave Packet ◽  
Transition State ◽  
State Wave

Mapping of transition‐state wave functions. II. A model for the photodissociation of ClNO(T1)

1992 ◽  
Vol 96 (5) ◽  
pp. 3688-3695 ◽  
Author(s):  
Aliki Vegiri ◽  
Agathe Untch ◽  
Reinhard Schinke
Keyword(s):  
Transition State ◽  
Wave Functions ◽  
State Wave

Mapping of parent transition‐state wave functions into product rotations: An experimental and theoretical investigation of the photodissociation of FNO

1992 ◽  
Vol 96 (9) ◽  
pp. 6643-6653 ◽  
Author(s):  
Amy Ogai ◽  
James Brandon ◽  
Hanna Reisler ◽  
Hans Ulrich Suter ◽  
J. Robert Huber ◽  
...  
Keyword(s):  
Transition State ◽  
Theoretical Investigation ◽  
Wave Functions ◽  
State Wave

Transition state wave packet study of hydrogen diffusion on Cu(100) surface

1999 ◽  
Vol 111 (13) ◽  
pp. 5741-5753 ◽  
Author(s):  
Dong H. Zhang ◽  
John C. Light ◽  
Soo-Y. Lee
Keyword(s):  
Wave Packet ◽  
Transition State ◽  
Hydrogen Diffusion ◽  
State Wave

scholarly journals The Effect of Topography on Storm-Track Intensity in a Relatively Simple General Circulation Model

2009 ◽  
Vol 66 (2) ◽  
pp. 393-411 ◽  
Author(s):  
Seok-Woo Son ◽  
Mingfang Ting ◽  
Lorenzo M. Polvani
Keyword(s):  
General Circulation ◽  
Wave Packets ◽  
Storm Track ◽  
Circulation Model ◽  
Equation Model ◽  
Storm Tracks ◽  
Background Flow ◽  
Primitive Equation ◽  
State Wave ◽  
Single Jet

Abstract The effect of topography on storm-track intensity is examined with a set of primitive equation model integrations. This effect is found to be crucially dependent on the latitudinal structure of the background flow impinging on the topography. If the background flow consists of a weak double jet, higher topography leads to an intensification of the storm track downstream of the topography, consistent with enhanced baroclinicity in that region. However, if the background flow consists of a strong single jet, topography weakens the storm track, despite the fact that the baroclinicity downstream of the topography is again enhanced. The different topographic impact results from the different wave packets in the two background flows. For a weak double-jet state, wave packets tend to radiate equatorward and storm-track eddies grow primarily at the expense of local baroclinicity. In contrast, for a strong single-jet state, wave packets persistently propagate in the zonal direction and storm tracks are affected not only by local baroclinicity but also by far-upstream disturbances via downstream development. It is the reduction of the latter by the topography that leads to weaker storm tracks in a strong single-jet state. The implications of these findings for Northern Hemisphere storm tracks are also discussed.

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