Grid scheduling divisible loads from two sources

Dimensioning and on-line scheduling in L

Dimensioning and on-line scheduling in Lambda Grids using divisible load concepts

✍ Pieter Thysebaert; Bruno Volckaert; Marc De Leenheer; Filip De Turck; Bart Dhoed 📂 Article 📅 2007 🏛 Springer US 🌐 English ⚖ 630 KB

The User-Level Scheduling of Divisible L

The User-Level Scheduling of Divisible Load Parallel Applications With Resource Selection and Adaptive Workload Balancing on the Grid

✍ Korkhov, V.V.; Moscicki, J.T.; Krzhizhanovskaya, V.V. 📂 Article 📅 2009 🏛 Institute of Electrical and Electronics Engineers 🌐 English ⚖ 746 KB

[IEEE 2004 IEEE 35th Annual Power Electr

[IEEE 2004 IEEE 35th Annual Power Electronics Specialists Conference - Aachen, Germany (20-25 June 2004)] 2004 IEEE 35th Annual Power Electronics Specialists Conference (IEEE Cat. No.04CH37551) - A new generalized two-stage direct power conversion topology to independently supply multiple AC loads from multiple power grids with adjustable power loading

✍ Klumpner, C.; Blaabjerg, F. 📂 Article 📅 2004 🏛 IEEE 🌐 English ⚖ 486 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