Vorträge
Vorträge 441 bis 450 von 746 | Gesamtansicht
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| Datum | Zeit | Ort | Vortrag |
|---|---|---|---|
| 21.04.17 | 09:00 | H 0.06 |
Approximation of Spectra and Pseudospectra on a Hilbert Space [Promotionsvortrag] Torge Schmidt |
| 03.04.17 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Using neural networks to classify paths in two-dimensional environments [Bachelorarbeit] Kieron Kretschmar, TM-Student |
| 31.03.17 | 14:00 | H0.03 |
Efficient and Accurate Evaluation of Aggregation Integrals in Population Balance Equations (Promotionsvortrag) Lusine Shahmuradyan |
| 27.03.17 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Numerische Simulation eines Modells einer Heißwasserhydrolyse (Bachelorarbeit) Thorben Abel |
| 28.02.17 | 10:00 | H 0.08 |
Minimierung des kleinsten Eigenwerts für Laplace-Operatoren auf metrischen Graphen [Bachelorarbeit] Yannick Jean Paul Lucien Saive, TM-Student |
| 15.02.17 | 11:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Präkonditionierer basierend auf filternden Matrix-Zerlegungen (Bachelorvortrag) Rasmus Wormstädt |
| 06.02.17 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Solving PDEs Numerically: RBF Collocation and Finite Volume Methods for Semiconductor Problems Dr. Patricio Farrell, Weierstrass Institut, Berlin Partial differential equations model a wide range of physical phenomena. |
| 26.01.17 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
The need for linear system solvers in dispersive wave modeling* Jörn Behrens, UHH Tsunami modeling is - to first (and very accurate) approximation - performed with the help of shallow water theory and equations. This is still the method of choice for many applications, including forecasting, hazard assessment and inundation modeling. However, for long propagation distances as well as highly nonuniform topographies dispersive effects become important. While truly dispersive model equations are fully three-dimensional and therefore expensive with respect to computational requirements, a common approach to dispersive modeling comprises a non-hydrostatic correction of shallow water equations. In order to derive this correction term, a linear system of equations needs to be solved in each time step - even when the time-stepping scheme is explicit. |
| 19.01.17 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Convergence of positive operator semigroups Moritz Gerlach, Universität Potsdam We give new conditions for strong convergence of positive operator |
| 15.12.16 | 14:00 | Am Schwarzenberg-Campus 3 (E), Raum 3.074 |
Optimierung von Pasteurisierungsprozessen Lea Versbach Ich werde in einem ca. 45 minütigen Vortrag meine Masterarbeit, die ich im Juni 2016 an der Uni Lund verteidigt habe, vorstellen. |
* Vortrag im Rahmen des Kolloquiums für Angewandte Mathematik





