Estimation of the most likely equilibrium traffic queueing pattern in a capacityconstrained network

The queue with flows of customers as a m

The queue with flows of customers as a model for traffic control in telecommunication networks

✍ Chesoong Kim; Sergey Dudin; Valentina Klimenok 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 936 KB

A column generation algorithm for the es

A column generation algorithm for the estimation of origin–destination matrices in congested traffic networks

✍ Ricardo García-Ródenas; Doroteo Verastegui-Rayo 📂 Article 📅 2008 🏛 Elsevier Science 🌐 English ⚖ 625 KB

A BRANCH-AND-BOUND/FLOW-EQUILIBRIUM ALGO

A BRANCH-AND-BOUND/FLOW-EQUILIBRIUM ALGORITHM FOR THE APPROXIMATE SOLUTION OF TOTAL COST MINIMIZATION PROBLEMS IN TRAFFIC NETWORKS

✍ Harry Böttcher; Werner Rothengatter; Bernd-Michael Sahling 📂 Article 📅 2005 🏛 Springer 🌐 English ⚖ 762 KB

Simultaneous estimation of the origin–de

Simultaneous estimation of the origin–destination matrices and the parameters of a nested logit model in a combined network equilibrium model

✍ Ricardo García-Ródenas; Ángel Marín 📂 Article 📅 2009 🏛 Elsevier Science 🌐 English ⚖ 609 KB

The global network of plate boundaries c

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid-plate rotations. Subduction is distributed along a single, long subnetwork, hence organizing the mantle convection as a single, long downwelling wall and two lower mantle upwelling columns, at the Pacific and African sides of the Earth, respectively. The columns should merge upward between Antarctica and Australia to reach the single, long spreading subnetwork. The flow encircles two toric volumes that escape convectional mixing and are the likely sources of the two, Atlantic–Indian and Pacific, hot spot domains.

✍ L.-E. Ricou 📂 Article 📅 1998 🏛 John Wiley and Sons 🌐 English ⚖ 197 KB

The global network of plate boundaries can be divided into two discrete subnetworks containing the spreading and subduction boundaries, respectively. We advocate that this division is a stable pattern that derives from consistency rules in rigid‐plate rotations. Subduction is distributed along a sin