Linear Response Function for Coupled Hyperbolic Attractors

2005 ◽  
Vol 261 (2) ◽  
pp. 379-404 ◽  
Author(s):  
Miaohua Jiang ◽  
Rafael de la Llave
Keyword(s):  
Response Function ◽  
Linear Response ◽  
Linear Response Function ◽  
Hyperbolic Attractors

Unified linear response function for zonal flows with full finite orbit effects

2007 ◽  
Vol 14 (11) ◽  
pp. 112512 ◽  
Author(s):  
T. Watari ◽  
Y. Hamada ◽  
A. Nishizawa ◽  
J. Todoroki
Keyword(s):  
Response Function ◽  
Linear Response ◽  
Zonal Flows ◽  
Linear Response Function

Extension of the linear response function of electron density to a plane-wave basis and the first application to periodic surface systems

2021 ◽  
Author(s):  
Tomohiro Maruyama ◽  
Jinta Ohnari ◽  
Kohei Tada ◽  
Yoyo Hinuma ◽  
Takashi Kawakami ◽  
...  
Keyword(s):  
Plane Wave ◽  
Electron Density ◽  
Response Function ◽  
Linear Response ◽  
Periodic Surface ◽  
Linear Response Function

Analysis of the linear response function relatingALtoVBsfor individual substorms

1995 ◽  
Vol 100 (A10) ◽  
pp. 19155 ◽  
Author(s):  
Gerard T. Blanchard ◽  
Robert L. McPherron
Keyword(s):  
Response Function ◽  
Linear Response ◽  
Linear Response Function

Macroturbulence Response to Vertical Stratification Change Using Linear Response Function of an Idealized Dry Atmosphere

2020 ◽  
Author(s):  
Pak-Wah Chan ◽  
Pedram Hassanzadeh ◽  
Zhiming Kuang
Keyword(s):  
Response Function ◽  
Linear Response ◽  
Momentum Flux ◽  
Pearson Correlation ◽  
Vertical Stratification ◽  
Near Surface ◽  
Zonal Scale ◽  
Linear Response Function ◽  
Zonal Wavenumber ◽  
Scaling Arguments

<p>Rossby radius and Rhines scale are two popular scaling arguments for eddy length scale. They have not been tested in a well-controlled experiment with increased vertical stratification and unchanged jet. This is done using the linear response function of an idealized dry atmosphere calculated by Hassanzadeh and Kuang (2016). The resulting change in zonal wind is mostly less than 0.2m/s when temperature near surface is cooled by more than 2K. In such experiment, energy-containing zonal scale decreases, which is against the prediction of Rossby radius but consistent with the prediction of Rhines scale. Eddy kinetic energy decreases for all wavenumbers and latitudes, but eddy momentum flux strengthens locally around zonal wavenumber 8 and 40°S. This local strengthening is associated with a stronger Pearson correlation between u and v.</p>

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