Dimensjonerende nedbørforløp for små urbane nedbørsfelt
The genesis of Norway’s largest staurolite crystals of the Fjordvangen-Nesoddtangen Supracrustal Complex and its implication for the Sveconorwegian orogenesis
Structural Analysis of the Øygarden Fault Complex, on the northern North Sea, Horda Platform
Simulating fluid flow surrounding carbonate fault zone
Hydrogeological study of Strømbo waterworks, Øvre Eiker municipality, Norway
Influence of forest on snow properties in Oslo, Norway
Secondary processes in the pegmatites of the Larvik Plutonic Complex, Norway
Morphologies and gas emissions from the Shamakhy-Gobustan mud volcano region, Azerbaijan
Identification and Characterization of Faults Using Deep Learning
Fault interpretation in high-resolution P-cable seismic data - Hoop Fault Complex
Sustainability and degradation of chemical deicers in the Gardermoen Aquifer: Iron and manganese redox processes
De-risking of faults associated with picking strategies: Implications for assessing fault growth and reactivation potential for CO2 storage in the Northern Horda Platform
Probabilistic analysis of quick clay slopes in Moss
Reconstructing possible causes for the darkening of Skagerrak coastal water in the Hvaler estuary during the past century.
Detecting land subsidence using multicriteria decision analysis and machine learning in Skøyen, Oslo
Feature detection in glacial channels using drifters (sic)
Qualitative and quantitative study of known exoplanets and exoplanetary systems.
Prediksjon av mettet infiltrasjonsrate ved bruk av fjernmåling og nevrale nett.
Isolating the influence of sea ice on Arctic warming in NorESM2.
Reconstruction of the marine paleoenvironment and paleoecology of the middle Holocene in the Oslo fjord area.
Low-frequency wave propagation in an ice-covered Arctic Ocean. Modeling with the spectral element package SPECFEM2D.
Infrastructure exposure to shallow landslides in Upper Gudbrandsdalen; Predicting the impact of climate change using the TRIGRS and RAMMS models.
The vertical structure of currents in Arctic and sub-Arctic regions.
Direct Solution for Closed f /H Contour Dynamics in High Latitude Ocean Basins.