V
Vladan Vučković
Researcher at University of Belgrade
Publications - 28
Citations - 353
Vladan Vučković is an academic researcher from University of Belgrade. The author has contributed to research in topics: Cloud seeding & Orography. The author has an hindex of 11, co-authored 26 publications receiving 332 citations. Previous affiliations of Vladan Vučković include University of Novi Sad.
Papers
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Journal ArticleDOI
Field-oriented control of induction machines in the presence of magnetic saturation
Emil Levi,Vladan Vučković +1 more
TL;DR: In this paper, field-oriented control principles are applied on the saturated model of induction machine and new equations are obtained, which differ significantly from the well-known model valid when the main flux saturation is absent or neglected.
Proceedings ArticleDOI
Saturation compensation schemes for vector controlled induction motor drives
TL;DR: In this paper, modifications that are necessary in the structures of rotor flux computers and indirect vector controllers in order to take into account the main flux saturation are considered, based on measurement of the stator currents, stator voltages and stator current, and rotor speed.
Journal ArticleDOI
Cloud seeding impact on precipitation as revealed by cloud-resolving mesoscale model
TL;DR: A cloud-resolving mesoscale model has been used to investigate the effects of cloud seeding by silver-iodide (AgI) if the seeding is performed at cold part of a long-lasting convective cloud as discussed by the authors.
Journal ArticleDOI
The effects of a river valley on an isolated cumulonimbus cloud development
TL;DR: In this article, the authors investigated the mechanism of development, propagation and front-side cell regeneration of a three-dimensional isolated cumulonimbus (Cb) cloud by a cloud-resolving mesoscale model.
Journal ArticleDOI
The influence of merging and individual storm splitting on mesoscale convective system formation
TL;DR: In this paper, the authors simulate the formation of mesoscale convective system (MCS) through splitting and merging of two single convective storms that is characteristic for mountainous regions by help of cloud-resolving model.