scholarly journals Multiscale sampling model for motion integration

2013 ◽  
Vol 13 (11) ◽  
pp. 18-18
Author(s):  
L. Sherbakov ◽  
A. Yazdanbakhsh
Keyword(s):  
Motion Integration ◽  
Multiscale Sampling

scholarly journals Bifurcation analysis applied to a model of motion integration with a multistable stimulus

2012 ◽  
Vol 34 (1) ◽  
pp. 103-124 ◽  
Author(s):  
James Rankin ◽  
Émilien Tlapale ◽  
Romain Veltz ◽  
Olivier Faugeras ◽  
Pierre Kornprobst
Keyword(s):  
Bifurcation Analysis ◽  
Motion Integration

scholarly journals Boundaries on motion integration

10.1038/89449 ◽  
2001 ◽  
Vol 4 (7) ◽  
pp. 680-680
Author(s):  
Josh McDermott
Keyword(s):  
Motion Integration

scholarly journals Motion integration across differing image features

1995 ◽  
Vol 35 (15) ◽  
pp. 2137-2146 ◽  
Author(s):  
Maggie Shiffrar ◽  
Xiaojun Li ◽  
Jean Lorenceau
Keyword(s):  
Image Features ◽  
Motion Integration

scholarly journals Different time scales of motion integration for anticipatory smooth pursuit and perceptual adaptation

2015 ◽  
Vol 15 (2) ◽  
pp. 16-16 ◽  
Author(s):  
G. W. Maus ◽  
E. Potapchuk ◽  
S. N. J. Watamaniuk ◽  
S. J. Heinen
Keyword(s):  
Time Scales ◽  
Smooth Pursuit ◽  
Perceptual Adaptation ◽  
Motion Integration ◽  
Different Time Scales

scholarly journals Marine Rapid Environmental Assessment in the Gulf of Taranto: a multiscale approach

2016 ◽  
Vol 16 (12) ◽  
pp. 2623-2639 ◽  
Author(s):  
Nadia Pinardi ◽  
Vladyslav Lyubartsev ◽  
Nicola Cardellicchio ◽  
Claudio Caporale ◽  
Stefania Ciliberti ◽  
...  
Keyword(s):  
Surface Waters ◽  
Large Scale ◽  
Eastern Mediterranean ◽  
Small Scale ◽  
Multiscale Approach ◽  
Mesoscale Variability ◽  
Large Scale Circulation ◽  
Eddy Field ◽  
Multiscale Sampling ◽  
Circulation Structure

Abstract. A multiscale sampling experiment was carried out in the Gulf of Taranto (eastern Mediterranean) providing the first synoptic evidence of the large-scale circulation structure and associated mesoscale variability. The mapping of the mesoscale and large-scale geostrophic circulation showed the presence of an anticyclonic large-scale gyre occupying the central open ocean area of the Gulf of Taranto. On the periphery of the gyre upwelling is evident where surface waters are colder and saltier than at the center of the gyre. Over a 1-week period, the rim current of the gyre undergoes large changes which are interpreted as baroclinic–barotropic instabilities, generating small-scale cyclonic eddies in the periphery of the anticyclone. The eddies are generally small, one of which can be classified as a submesoscale eddy due to its size. This eddy field modulates the upwelling regime in the gyre periphery.

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