Prosjekter
Publikasjoner
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Vitenskapelig artikkelFlood modeling prior to the instrumental era reveals limited magnitude of 1931 Yangtze flood– npj Climate and Atmospheric Science 2025
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Vitenskapelig artikkelUsing deep learning to understand flood variability across the last millennium from GCM atmospheric variables in two contrasting catchments– Journal of Hydrology 2025
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Vitenskapelig artikkelEnhanced Simulation of Atmospheric Blocking in a High-Resolution Earth System Model: Projected Changes and Implications for Extreme Weather Events– Journal of Geophysical Research (JGR): Atmospheres 2025
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Vitenskapelig artikkelMore high-impact atmospheric river-induced extreme precipitation events under warming in a high-resolution model– One Earth 2024
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Vitenskapelig artikkelWarm Advection as a Cause for Extreme Heat Event in North China– Geophysical Research Letters 2024
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Vitenskapelig artikkelObservations of Parametric Subharmonic Instability of Diurnal Internal Tides in the Northwest Pacific– Journal of Physical Oceanography 2024
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Vitenskapelig artikkelModeled variations of tropical cyclone genesis potential during Marine Isotope Stage 3– Quaternary Science Reviews 2024
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Vitenskapelig artikkelThe hydrological cycle and ocean circulation of the Maritime Continent in the Pliocene: results from PlioMIP2– Climate of the Past 2023
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Vitenskapelig oversiktsartikkelArctic Ocean simulations in the CMIP6 Ocean Model Intercomparison Project (OMIP)– Geoscientific Model Development 2023
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KonferanseforedragInfluence of global mean sea-level rise on atmospheric and oceanic circulations– IUGG 2023, General Assemblies, 1 General, International Union of Geodesy and Geophysics (IUGG) 2023
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Vitenskapelig artikkelDansgaard–Oeschger events in climate models: review and baseline Marine Isotope Stage 3 (MIS3) protocol– Climate of the Past 2023
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KonferanseforedragOcean-sea ice dynamics in the Nordic Seas across a stadial-interstadial transition – a modelling and data perspective– XXI INQUA Congress 2023
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Vitenskapelig artikkelAtlantic circulation changes across a stadial-interstadial transition– Climate of the Past 2023
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KonferanseforedragABRUPT Arctic Climate Change– EGU 2023 2023
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Vitenskapelig artikkelAtmospheric and oceanic circulation altered by global mean sea-level rise– Nature Geoscience 2023
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Vitenskapelig artikkelUnraveling the mechanisms and implications of a stronger mid-Pliocene Atlantic Meridional Overturning Circulation (AMOC) in PlioMIP2– Climate of the Past 2023
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Vitenskapelig artikkelRecognizing the Role of Tropical Seaways in Modulating the Pacific Circulation– Geophysical Research Letters 2022
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KonferanseforedragCMIP6/OMIP simulations of the Arctic Ocean and Resolution effects– international symposium in remembrance of Prof. Yongqi Gao: The Ocean, Sea Ice and Northern Hemisphere Climate 2022
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KonferanseforedragCMIP6/OMIP simulations of the Arctic Ocean and introduction of KeyPOCP project– China-Norway Marine University Consortium Alliance Annual Academic Conference 2022 (CNMU Conference 2022) 2022
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Vitenskapelig artikkelPast terrestrial hydroclimate sensitivity controlled by Earth system feedbacks– Nature Communications 2022
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Vitenskapelig artikkelWidespread glacier advances across the Tian Shan during Marine Isotope Stage 3 not supported by climate-glaciation simulations– Fundamental Research 2022
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Vitenskapelig artikkelMid-Pliocene West African Monsoon rainfall as simulated in the PlioMIP2 ensemble– Climate of the Past 2021
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Vitenskapelig artikkelMid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2– Climate of the Past 2021
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Vitenskapelig artikkelReduced El Niño variability in the mid-Pliocene according to the PlioMIP2 ensemble– Climate of the Past 2021
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Vitenskapelig artikkelEvaluating the large-scale hydrological cycle response within the Pliocene Model Intercomparison Project Phase 2 (PlioMIP2) ensemble– Climate of the Past 2021
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Vitenskapelig artikkelNorCPM1 and its contribution to CMIP6 DCPP– Geoscientific Model Development 2021
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Vitenskapelig artikkelLarge-scale features of Last Interglacial climate: results from evaluating the lig127k simulations for the Coupled Model Intercomparison Project (CMIP6)–Paleoclimate Modeling Intercomparison Project (PMIP4)– Climate of the Past 2021
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Vitenskapelig artikkelA multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences– Climate of the Past 2021
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Vitenskapelig artikkelLarge-scale features and evaluation of the PMIP4-CMIP6 midHolocene simulations– Climate of the Past 2020
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Vitenskapelig artikkelComparison of past and future simulations of ENSO in CMIP5/PMIP3 and CMIP6/PMIP4 models– Climate of the Past 2020
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Vitenskapelig artikkelGlobal River Discharge and Floods in the Warmer Climate of the Last Interglacial– Geophysical Research Letters 2020
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Vitenskapelig artikkelOverview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations– Geoscientific Model Development 2020
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Vitenskapelig artikkelEvaluation of global ocean-sea-ice model simulations based on the experimental protocols of the Ocean Model Intercomparison Project phase 2 (OMIP-2)– Geoscientific Model Development 2020
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Vitenskapelig artikkelPast perspectives on the present era of abrupt Arctic climate change– Nature Climate Change 2020
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Vitenskapelig artikkelThe Pliocene Model Intercomparison Project Phase 2: large-scale climate features and climate sensitivity– Climate of the Past 2020
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Vitenskapelig artikkelLessons from a high-CO2 world: an ocean view from ∼ 3 million years ago– Climate of the Past 2020
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Vitenskapelig artikkelEvaluation of Arctic warming in mid-Pliocene climate simulations– Climate of the Past 2020
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Vitenskapelig artikkelPlioMIP2 simulations with NorESM-L and NorESM1-F– Climate of the Past 2020
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Vitenskapelig artikkelAgreement between reconstructed and modeled boreal precipitation of the Last Interglacial– Science Advances 2019
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KonferanseforedragDynamical sequence of ocean, atmosphere, and sea ice changes during an abrupt stadial-to-interstadial climate transition– American Geophysical Union (AGU) 2019
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KonferanseforedragThe dynamics of abrupt climate changes during the last glacial cycle– European Geophysical Union 2019
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Vitenskapelig artikkelEquilibrium simulations of Marine Isotope Stage 3 climate– Climate of the Past 2019
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Vitenskapelig artikkelSeasonal and Spatial Variations of the M2 Internal Tide in the Yellow Sea– Journal of Geophysical Research (JGR): Space Physics 2019
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KonferanseforedragThe Dynamics of DO-events– LSCE workshop 2019
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Vitenskapelig artikkelDescription and evaluation of NorESM1-F: a fast version of the Norwegian Earth System Model (NorESM)– Geoscientific Model Development 2019
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Vitenskapelig artikkelInstability of Northeast Siberian ice sheet during glacials– Climate of the Past 2018
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Vitenskapelig artikkelEemian Greenland SMB strongly sensitive to model choice– Climate of the Past 2018
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KonferanseforedragEemian Greenland Surface Mass Balance strongly sensitive to SMB model setup– EGU General Assembly 2018 2018
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Vitenskapelig artikkelAtlantic deep water circulation during the last interglacial– Scientific Reports 2018
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KonferanseforedragThe Atlantic deep water circulation during the last interglacial– Ocean Sciences Meeting 2018 2018
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KonferanseforedragAbrupt climate changes during a stadial to interstadial transition– Ice2ice all-staff meeting 2018
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KonferanseforedragThe Norwegian Earth System Model: Framework, Application, and CMIP6 involvement– International Coupled Data Assimilation Symposium 2017
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Vitenskapelig artikkelCharacteristics of the Nordic Seas overflows in a set of Norwegian Earth System Model experiments– Ocean Modelling 2016
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Vitenskapelig artikkelOn the modulation of the periodicity of the Faroe Bank Channel overflow instabilities– Ocean Science 2015
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Vitenskapelig artikkelBaroclinic instability of the Faroe Bank Channel overflow– Journal of Physical Oceanography 2014
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Vitenskapelig artikkelCombined effect of rotation and topography on shoaling oceanic internal solitary waves– Journal of Physical Oceanography 2014
