scholarly journals The log–linear response function of the bounded number-line task is unrelated to the psychological representation of quantity

2017 ◽  
Vol 25 (1) ◽  
pp. 447-454 ◽  
Author(s):  
Dale J. Cohen ◽  
Philip T. Quinlan
Keyword(s):  
Response Function ◽  
Linear Response ◽  
Number Line ◽  
Bounded Number ◽  
Linear Response Function ◽  
Log Linear

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

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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