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Arrangementer - Side 12

Tid og sted: , Digital examination, Zoom

Secondary processes in the pegmatites of the Larvik Plutonic Complex, Norway

Tid og sted: , Room 2414 Kristine Bonnevies hus

Title: Multiscale interactions in the Labrador Sea: from submesoscale circulations to climate scales

Speaker: Annalisa Bracco, Georgia Institute of Technology

Tid og sted: , Aud 1, Geologibygningen

Ph.d.-kandidat Marta Trodahl ved Institutt for geofag, Det matematisk-naturvitenskapelige fakultet, vil forsvare avhandlingen Vortices in the Subarctic Seas and their interactions with bottom topography for graden Philosophiae Doctor.

Tid og sted: , Aud. 2, the Geology building, University of Oslo

Morphologies and gas emissions from the Shamakhy-Gobustan mud volcano region, Azerbaijan

Tid og sted: , Digital examination, Zoom

Identification and Characterization of Faults Using Deep Learning

Tid og sted: , Meeting room K43 (Bifrost), the Geology building, University of Oslo

Fault interpretation in high-resolution P-cable seismic data - Hoop Fault Complex

Tid:

Title: How consistent are observed and simulated records of volcanic eruptions?

Speaker: Gabi Hegerl, University of Edinburgh

Tid og sted: , Aud. 2, the Geology building, University of Oslo

Sustainability and degradation of chemical deicers in the Gardermoen Aquifer: Iron and manganese redox processes

Tid og sted: , Digital examination, Zoom

De-risking of faults associated with picking strategies: Implications for assessing fault growth and reactivation potential for CO2 storage in the Northern Horda Platform

Tid og sted: , Seminar room 219 (Valhall), the Geology building, University of Oslo

Probabilistic analysis of quick clay slopes in Moss

Tid og sted: , The Geology building, room 219, Valhall

Reconstructing possible causes for the darkening of Skagerrak coastal water in the Hvaler estuary during the past century.

Tid og sted: , Digital examination, Zoom

Detecting land subsidence using multicriteria decision analysis and machine learning in Skøyen, Oslo

Tid og sted: , The Geology building, Room 219 Valhall

Feature detection in glacial channels using drifters (sic)

Tid og sted: , Digital - Zoom

Qualitative and quantitative study of known exoplanets and exoplanetary systems.

Tid og sted: , Bruun room/met.no

Title: Accelerating climate science with machine learning: Earth system emulation

Speaker: Duncan Watson-Parris, University of Oxford

Tid og sted: , The Geology building, Room 219

Prediksjon av mettet infiltrasjonsrate ved bruk av fjernmåling og nevrale nett.

Tid og sted: , The Kristine Bonnevies building, MetOs, room 2320

Isolating the influence of sea ice on Arctic warming in NorESM2.

Tid og sted: , Aud 1, Geologibygningen

Ph.d.-kandidat Md Jamilur Rahman ved Institutt for geofag, Det matematisk-naturvitenskapelige fakultet, vil forsvare avhandlingen Seal, and overburden rock characterization of potential CO2 storage sites in the northern North Sea for graden Philosophiae Doctor.

Tid og sted: , Natural History Museum/NHM, Room U540, Økern

Reconstruction of the marine paleoenvironment and paleoecology of the middle Holocene in the Oslo fjord area.

Tid og sted: , The Geology building, Aud 2

Low-frequency wave propagation in an ice-covered Arctic Ocean. Modeling with the spectral element package SPECFEM2D.

Tid og sted: , The Geology building, Room 219 Valhall

Infrastructure exposure to shallow landslides in Upper Gudbrandsdalen; Predicting the impact of climate change using the TRIGRS and RAMMS models.

Tid og sted: , The Kristine Bonnevies building, Rom 2414

The vertical structure of currents in Arctic and sub-Arctic regions.

Tid og sted: , The Kristine Bonnevies building, Room 2414

Direct Solution for Closed f /H Contour Dynamics in High Latitude Ocean Basins.

Tid og sted: , The Geology building, Room 219 Valhall

Estimering av Snøens Vannekvivalent i Nord-Amerika med Undersøkelse av Generaliseringsfeil med XGBoost og Random Forest.

Tid og sted: , Zoom (videolink), the main supervisor sends invitation.

Hydrous Regions of the Mantle Transition Zone Affect Patterns of Intraplate Volcanism.