[Forschungsseminar-BSV] Research Seminar 'Computer Graphics, Image Processing, and Visualization'
Tom Liebmann
liebmann at informatik.uni-leipzig.de
Mo Mai 29 11:53:39 CEST 2017
I N V I T A T I O N
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to the Research Seminar 'Computer Graphics, Image Processing, and Visualization'
on Thursday, June 1st, 2017, at 1:15 PM,
in Room P-702 in the Paulinum, Augustusplatz.
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There will be two talks. The first one is given by
Pascal Nardini
Image and Signal Processing Group
Department of Computer Science
Leipzig University
and is entitled
"Visual Study of the Benguela Upwelling System using Pathline Predicates".
Abstract:
Due to the nutrient-rich water transported to the upper layer of the ocean,
coastal upwelling systems are regions especially important for marine life
and fishery. In this work, we focus on a visual analysis of the
spatio-temporal structure of the Benguela upwelling system using pathline
predicates. Based on the 3D flow field from an ocean model simulation, we
first derive space-filling trajectories covering the full model grid. From
these, we select and visualize pathlines related to upwelling. In a second
step, we derive a 3D scalar field representing the pathline density, which
is visualized using volume rendering techniques. Further analyses of the
pathlines show a distinct annual cycle in the upwelling activity, which
fits well to observation-based analyses found in literature.
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The second talk is given by
Felix Raith
Image and Signal Processing Group
Department of Computer Science
Leipzig University
and is entitled
"Visual Eddy Analysis of the Agulhas Current".
Abstract:
Large mesoscale eddies in the ocean can transport a substantial amount of
heat and salt over large distances. Using high-resolution ICON ocean
simulation data, it is possible to detect and track eddies in the ocean and
analyze their pathway. In this paper, we focus on the area of the Agulhas
Current at the southern tip of Africa and present our results for eddy
detection and eddy tracking. The Agulhas Current transports warm and salty
water from the Indian Ocean towards the South Atlantic Ocean before it
makes a strong turn back into the Indian Ocean. Some eddies associated with
this current do not follow this turn back into the Indian Ocean, but travel
north-west deeper up the Atlantic. We show how such eddies can be detected
and tracked in the ICON model and how far some of them travel over the
duration of one year. We also indicate which types of eddies follow these
paths and give a visual analysis of eddy properties like volume and
temperature.
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On behalf of Professor Scheuermann all those interested are cordially invited to attend.
Yours sincerely,
Tom Liebmann
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