Tidlegare gjesteforelesninger og seminarer - Side 85

Tid og stad: , Room 3508

Friday seminar by James D. Nichols

Tid og stad: , The National Library
Tid og stad: , Room 3508

Friday Seminar by Frans de Waal

Tid og stad: , Room 3508

Extra CEES seminar by Hal Caswell

Tid og stad: , B91

Aleksey Marchenko is professor and departemental leader for the UNIS Arctic Technology department

Tid og stad: , Room 3315, Kristine Bonnevies hus

Extra seminar by Elisabeth Beaubien, founder of Plantwatch Canada

Tid og stad: , Store fysiske auditorium, Fysikkbygningen
Tid og stad: , Room 3508

Friday seminar by Mikael Ohlson.

Tid og stad: , Room 3508

Friday seminar by Reidun Sirevåg

Tid og stad: , Seminarrom 231, Helga Engs hus
Tid og stad: , Room 3508

Friday seminar by Rebecca Kilner

Tid og stad: , Room 3315

Extra CEES seminar by Eric Chivian

Tid og stad: , Room 3508

Friday seminar by John Buonaccorsi

Tid og stad: , lounge area, 9th floor, Abel bld

Main advantages and challenges of using Domain-Decomposition (DD) strategies for marine applications are examined. Splitting algorithms are discussed with emphasis on the spatial DD. Examples are given for platform and ship problems in connection with bottom-slamming and green-water occurrence. Features of the involved DD strategies are described and relevant verification and validation studies reported.

Marilena Greco is professor at Department of Marine hydrodynamics at NTNU

Tid og stad: , Room 3508

Friday seminar by Philipp Mitteröcker

Tid og stad: , Room 3508

Friday seminar by Hans Heesterbeek

Tid og stad: , B91

Oscillating boundary layers in the ocean are of fundamental interest as they are important in phenomena such as mixing, sediment transport and drift mechanisms. These boundary layers occur on different time and length scales. The waves induce a thin layer near the surface, and, for intermediate and shallow water depths, an oscillatory bottom boundary layer. The gravity forces from the moon and the sun, in conjunction with the Earths rotation, induces tidal boundary layers. Oscillatory boundary layers often result from an interaction between the oscillatory motion and a current, for example induced by wind at the ocean surface. In general these boundary layers are turbulent in the ocean, and it will be shown how these boundary layers can be calculated using a relative simple two-equation turbulence model. Results from an ongoing work considering the entire water column for a tidal flow with wind at the surface will be given. Finally a few preliminary LES test results from channel flow, from our development of LES codes, will be presented, and a brief discussion of some problems which we expect to face when using these models on geophysical flows will be given.

Lars Erik Holmedal is researcher at Department of Marine Technology, NTNU

Tid og stad: , Aud. 3, Kristine Bonnevies hus (Biology Building), Blindern

Friday seminar by Yohannes Haile-Selassie.