Results 1 to 10 of about 3,840,075 (194)
The upper edge geodetic number and the forcing edge geodetic number of a graph [PDF]
An edge geodetic set of a connected graph \(G\) of order \(p \geq 2\) is a set \(S \subseteq V(G)\) such that every edge of \(G\) is contained in a geodesic joining some pair of vertices in \(S\).
A. P. Santhakumaran, J. John
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Single coronoid systems with an anti-forcing edge
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Heping Zhang
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Forcing and anti-forcing edges in bipartite graphs
Let G be a connected bipartite graph with a perfect matching and the minimum degree at least two. The concept of an anti-forcing edge in G was introduced by Li in Li (1997). One known generalized version for an anti-forcing edge is an anti-forcing set S ,
Zhongyuan Che, Zhibo Chen
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Forcing edge detour monophonic number of a graph [PDF]
For a connected graph $G=(V,E)$ of order at least two, an edge detour monophonic set of $G$ is a set $S$ of vertices such that every edge of $G$ lies on a detour monophonic path joining some pair of vertices in $S$. The edge detour monophonic number
P. Titus, K. Ganesamoorthy
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Hexagonal systems with forcing single edges
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Xueliang Li
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Optimizing large-scale graph database ingestion through edge value ranking: a proposed framework [PDF]
This paper proposes a preprocessing framework for optimizing large-scale graph database ingestion through intelligent edge filtering based on value ranking. We combine adapted PageRank algorithms with business-specific metrics and edge type importance to
Phanindra Reddy Madduru, Bijo Thomas
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Edge Forcing in Butterfly Networks [PDF]
A zero forcing set is a set $S$ of vertices of a graph $G$, called forced vertices of $G$, which are able to force the entire graph by applying the following process iteratively: At any particular instance of time, if any forced vertex has a unique unforced neighbor, it forces that neighbor.
G. Jessy Sujana +3 more
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Vertex and edge spread of zero forcing number, maximum nullity, and minimum rank of a graph
Christina J Edholm, Leslie Hogben
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The future of the El Niño–Southern Oscillation: using large ensembles to illuminate time-varying responses and inter-model differences [PDF]
Future changes in the El Niño–Southern Oscillation (ENSO) are uncertain, both because future projections differ between climate models and because the large internal variability of ENSO clouds the diagnosis of forced changes in observations and ...
N. Maher +11 more
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Extreme precipitation events have been occurring frequently worldwide, and their causative factors and convection initiation (CI) mechanisms have been attracting more and more attention in recent years.
Qi Sun +8 more
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