I am a research professor in the Earth System group at NORCE Climate & Environment and a member of the Bjerknes Centre for Climate Research. The objective of my research is to apply Earth system models and observations to advance our understanding and prediction of anthropogenic climate change; to model large scale ocean biogeochemical cycle and its interactions and feedback to the climate system from interannual to centennial time scales; to quantify the dominant internal climate variability and elucidating how they are affected by external forcings,such as carbon dioxide, volcanic eruptions, and large scale geoengineering; to determine and attribute sources of uncertainties leading to the large spread in climate models; to use observations and various statistical metrics to constraint and characterize model uncertainties and minimize projection errors. I am part of the Norwegian Earth System Model consortium and coordinate the development and maintenance of the ocean carbon cycle component.
Divisjon
Klima og miljø
Forskningstema
Forskergrupper
Mer info om Jerry
Prosjekter
Publikasjoner
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KonferanseforedragContrasting trends of marine bromoform emissions in a future climate– EGU General Assembly 2024
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Vitenskapelig artikkelAERA-MIP: emission pathways, remaining budgets, and carbon cycle dynamics compatible with 1.5 and 2 °C global warming stabilization– Earth System Dynamics (ESD) 2024
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KonferanseforedragWhat goes in must come out: the outgassing of anthropogenic CO2 from the ocean– AGU Annual meeting 2024 2024
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KonferanseforedragPersistent inter-model uncertainties in oceanic CO2 flux in past CMIPs and how to ameliorate them– AGU Annual meeting 2024 2024
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KonferanseforedragWhat goes in must come out: the oceanic outgassing of anthropogenic CO2– SOLAS Open science conference 2024
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Vitenskapelig artikkelAssessing the tropical Atlantic biogeochemical processes in the Norwegian Earth System Model– Biogeosciences 2024
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KonferanseforedragUncertainties in ocean biogeochemical projections and how to constrain them– CLIVAR and FIO summer school 2024
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KonferanseforedragOcean biogeochemical cycle representations in Earth system models– CLIVAR-FIO Summer school 2024
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KonferanseforedragMachine learning to constrain future ocean CO2 fluxes– CE2COAST final meeting 2024 2024
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Vitenskapelig artikkelNatural marine bromoform emissions in the fully coupled ocean-atmosphere model NorESM2– Earth System Dynamics (ESD) 2024
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KonferanseforedragCE2COAST: Case Study 7: Norway.– Norkyst Working Group meeting 2024
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Vitenskapelig artikkelProjected poleward migration of the Southern Ocean CO2 sink region under high emissions– Communications Earth & Environment 2024
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KonferanseforedragDigital twins of the Norwegian fjords: a decision support system– NORCE Climate and Environment conference 2024
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KonferanseforedragNon-intuitive contrast between Ninos-driven CO2 flux variability and long term changes in the tropical Atlantic and Pacific– EGU General Assembly 2024 2024
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KonferanseforedragImpacts of solar geoengineering on marine system– Korea-Norway exchange workshop 2024
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KonferanseforedragESMValTool-based validation and evaluation toolkit for ocean performance– CMCC-NorESM joint workshop 2024
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Vitenskapelig artikkelAn Assessment of CO2 Storage and Sea-Air Fluxes for the Atlantic Ocean and Mediterranean Sea Between 1985 and 2018– Global Biogeochemical Cycles 2024
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Vitenskapelig artikkelRadiative forcing geoengineering causes higher risk of wildfires and permafrost thawing over the Arctic regions– Communications Earth & Environment 2024
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Vitenskapelig artikkelMachine learning reveals regime shifts in future ocean carbon dioxide fluxes inter-annual variability– Communications Earth & Environment 2024
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Vitenskapelig artikkelMore Frequent Abrupt Marine Environmental Changes Expected– Geophysical Research Letters 2024
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Vitenskapelig artikkelWhat goes in must come out: the oceanic outgassing of anthropogenic carbon– Environmental Research Letters 2024
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Vitenskapelig artikkelCarbon cycle feedbacks in an idealized simulation and a scenario simulation of negative emissions in CMIP6 Earth system models– Biogeosciences 2024
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KonferanseforedragMultiyear phytoplankton predictability in the Barents Sea– The Arctic Science Summit Week 2023
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Vitenskapelig artikkelAn along-Track Biogeochemical Argo modelling framework: A case study of model improvements for the Nordic seas– Geoscientific Model Development 2023
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KonferanseforedragGlobal and regional marine bromoform emissions in a fully coupled ocean-atmosphere-model– EGU General Assembly 2023 2023
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KonferanseforedragLessons from COVID-19 emission reduction simulations with NorESM2– CACTI (Composition Air quality Climate inTeractions Initiative) workshop 2023 2023
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Vitenskapelig artikkelSimulations of ocean deoxygenation in the historical era: insights from forced and coupled models– Frontiers in Marine Science 2023
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KonferanseforedragOptimized observing network to detect anthropogenic signals in the ocean: insights from model projections– WCRP Open Science Conference 2023 2023
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KonferanseforedragTropical Atlantic: a hotspot for early detectable and long-lasting anthropogenic changes in ocean interior– PIRATA Conf. &TRIATLAS GA 2023
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KonferanseforedragEarth system model at regional scale– CE2COAST Annual meeting 2023 2023
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KonferanseforedragProfound impact of SRM on the marine system– 17th ASLLA Symposium 2023
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Vitenskapelig artikkelA Regime View of ENSO Flavors Through Clustering in CMIP6 Models– Earth's Future 2023
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Vitenskapelig artikkelDeep Ocean Circulation Governs Sedimentary CaCO<inf>3</inf> Accumulation in the Northeast Pacific Ocean– Journal of Geophysical Research (JGR): Oceans 2023
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Vitenskapelig artikkelIrreversible loss in marine ecosystem habitability after a temperature overshoot– Communications Earth & Environment 2023
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KonferanseforedragCarbon cycle feedbacks under negative emissions in CMIP6 Earth system models– Workshop on High-latitude Earth Climate System 2023
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Vitenskapelig artikkelSeasonal Variability of the Surface Ocean Carbon Cycle: A Synthesis– Global Biogeochemical Cycles 2023
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Vitenskapelig artikkelKey physical processes and their model representation for projecting climate impacts on subarctic Atlantic net primary production: A synthesis– Progress in Oceanography 2023
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Vitenskapelig artikkelDisentangling the impact of Atlantic Niño on sea-air CO<inf>2</inf> flux– Nature Communications 2023
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Vitenskapelig artikkelAtlantic circulation changes across a stadial-interstadial transition– Climate of the Past 2023
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Vitenskapelig artikkelPhytoplankton abundance in the Barents Sea is predictable up to five years in advance– Communications Earth & Environment 2023
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Vitenskapelig artikkelTrivial gain of downscaling in future projections of higher trophic levels in the Nordic and Barents Seas– Fisheries Oceanography 2023
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Vitenskapelig artikkelThe representation of alkalinity and the carbonate pump from CMIP5 to CMIP6 Earth system models and implications for the carbon cycle– Biogeosciences 2023
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Vitenskapelig artikkelGlobal Surface Ocean Acidification Indicators From 1750 to 2100– Journal of Advances in Modeling Earth Systems 2023
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KonferanseforedragDetection timescales of environmental stressors in the interior ocean– NorESM seminar series 2023
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KonferanseforedragIntroduction to iHAMOCC– OceanICU model introduction workshop 2023
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KonferanseforedragConstraining ocean carbon sink projections in CMIP6 models– EGU 2023 2023
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KonferanseforedragResponse of the ENSO-driven CO2 flux variability in the equatorial Pacific under high-warming scenario– EGU 2023 2023
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KonferanseforedragAn assessment of CO2 storage and sea-air fluxes of the Atlantic Ocean and Mediterranean Sea between 1985 and 2018– EGU 2023 2023
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KonferanseforedragDetecting anthropogenic climate change signals of marine stressors in the interior– ECCWO5 2023
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Vitenskapelig artikkelAdded value of a regional coupled model: the case study for marine heatwaves in the Caribbean– Climate Dynamics 2023
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Vitenskapelig artikkelThe emergence of the Gulf Stream and interior western boundary as key regions to constrain the future North Atlantic carbon uptake– Geoscientific Model Development 2023
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Vitenskapelig artikkelEarly detection of anthropogenic climate change signals in the ocean interior– Scientific Reports 2023
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Vitenskapelig artikkelRiverine impact on future projections of marine primary production and carbon uptake– Biogeosciences 2023
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KonferanseforedragSkillful Prediction of Barents Sea Phytoplankton Concentration– EGU General Assembly 2022 2022
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Vitenskapelig artikkelA scalable, black-box hybrid genetic algorithm for continuous multimodal optimization in moderate dimensions– Nordic Machine Intelligence (NMI) 2022
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KonferanseforedragCarbon cycle feedbacks in an idealized and a scenario simulation of carbon dioxide removal in CMIP6 Earth system models– EGU General Assembly 2022
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KonferanseforedragConstraining the large spread in ocean carbon sinks in ESMs– ECMWF 6th WGNE workshop on systematic errors in weather and climate models 2022
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KonferanseforedragEarth system model at regional scale– CE2COAST annual meeting 2022 2022
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KonferanseforedragIPCC-AR6 Ch5 Global biogeochemical cycles and climate feedback– Guest lecturer GEO4990 The Earth System 2022
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KonferanseforedragModeling the Eastern Tropical Pacific with COAWST, a coupled ocean-atmosphere model– EASMO - ICRS Meeting 2022
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KonferanseforedragClimate change in the Eastern Tropical Pacific ocean– Full EASMO consortium meeting 2022
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KonferanseforedragDeveloping a High Resolution Coupled Ocean-Atmospheric Model to Understand Reef Fish Distribution in the Eastern Tropical Pacific– Ocean Science Meeting 2022
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KonferanseforedragDeveloping a high resolution coupled ocean-atmospheric model to understand reef fish distribution in the Eastern Tropical Pacific in the present and future climate– EGU General Assembly 2022
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Vitenskapelig artikkelA functional vulnerability framework for biodiversity conservation– Nature Communications 2022
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KonferanseforedragMarine heat waves: The added value of a high resolution, coupled atmosphere-ocean regional climate model– EGU General Assembly 2022 2022
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ForskningsrapportTrender i havforsuring og antropogent karbon i de nordiske hav, Nordsjøen og Skagerrak– NORCE Norwegian Research Centre 2022
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KonferanseforedragDetection timescale of anthropogenic climate change signals in the global ocean– EGU 2022 2022
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Vitenskapelig artikkelContrasting projections of the ENSO-driven CO2 flux variability in the equatorial Pacific under high-warming scenario– Earth System Dynamics (ESD) 2022
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KonferanseforedragJet streams and storm tracks in global climate models: "understanding" uncertainty in future projections– Stormtracks2022 : Midlatitude storm-tracks workshop 2022
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KonferanseforedragGulf Stream and Deep Western Boundary Currents are key to constrain the future North Atlantic Carbon Uptake– EGU General Assembly 2022 2022
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KonferanseforedragGulf Stream and Deep Western Boundary Currents are key to constrain the future North Atlantic Carbon Uptake– EGU General Assembly 2022 2022
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KonferanseforedragGulf Stream and Deep Western Boundary Currents are key to constrain the future North Atlantic Carbon Uptake– EGU General Assembly 2022 2022
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Vitenskapelig artikkelBiogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing– Journal of Geophysical Research (JGR): Oceans 2022
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KonferanseforedragChanges in ENSO-driven CO2 flux variability in the Equatorial Pacific– Ocean Science Meeting 2022 2022
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Vitenskapelig artikkelEstimation of Ocean Biogeochemical Parameters in an Earth System Model Using the Dual One Step Ahead Smoother: A Twin Experiment– Frontiers in Marine Science 2022
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Vitenskapelig artikkelAcidification of the Nordic Seas– Biogeosciences 2022