scholarly journals Mixed Search Number and Linear-Width of Interval and Split Graphs

Author(s):  
Fedor V. Fomin ◽  
Pinar Heggernes ◽  
Rodica Mihai
Keyword(s):  
Networks ◽  
2009 ◽  
Vol 56 (3) ◽  
pp. 207-214 ◽  
Author(s):  
Fedor V. Fomin ◽  
Pinar Heggernes ◽  
Rodica Mihai
Keyword(s):  

2016 ◽  
Vol 32 (4) ◽  
pp. 1005-1014
Author(s):  
Jian-hua Yin ◽  
Lei Meng ◽  
Meng-Xiao Yin
Keyword(s):  

2021 ◽  
pp. 189-206
Author(s):  
Karen L. Collins ◽  
Ann N. Trenk
Keyword(s):  

Games ◽  
2021 ◽  
Vol 12 (3) ◽  
pp. 55
Author(s):  
Markus Kinateder ◽  
Luca Paolo Merlino

In this paper, we propose a game in which each player decides with whom to establish a costly connection and how much local public good is provided when benefits are shared among neighbors. We show that, when agents are homogeneous, Nash equilibrium networks are nested split graphs. Additionally, we show that the game is a potential game, even when we introduce heterogeneity along several dimensions. Using this result, we introduce stochastic best reply dynamics and show that this admits a unique and stationary steady state distribution expressed in terms of the potential function of the game. Hence, even if the set of Nash equilibria is potentially very large, the long run predictions are sharp.


2010 ◽  
Vol 39 (17) ◽  
Author(s):  
Sheila de Almeida ◽  
Celia de Mello ◽  
Aurora Morgana
Keyword(s):  

2015 ◽  
Vol 21 (3) ◽  
pp. 284-287
Author(s):  
Yumei Hu ◽  
Tingting Liu

1994 ◽  
Vol 52 (3) ◽  
pp. 307-312 ◽  
Author(s):  
Frédéric Maffray ◽  
Myriam Preissmann
Keyword(s):  

1997 ◽  
Vol 43 (145) ◽  
pp. 557-562 ◽  
Author(s):  
David B. Bahr

AbstractAn analysis of hundreds of mountain and valley glaciers in the former Soviet Union and the Alps shows that characteristic glacier widths scale as characteristic glacier lengths raised to an exponent of 0.6. This is in contrast to most previous analyses which implicitly of explicitly assumed scaling exponents of either 0 or 1. The exponent 0.6 implies that average glacier widths are proportional to average glacier thicknesses. Although this seems to suggest V-shaped glacier valleys, the linear width-thickness relationship is not inconsistent with parabolic valley cross-sections, because the characteristic (or average) width of a glacier depends on many other aspects of channel and glacier morphology, including variations in the channel width with distance up- and downstream.


2021 ◽  
Vol 8 (1) ◽  
pp. 120-124
Author(s):  
Xuan Hung Xuan Hung
Keyword(s):  

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