I have a broad background in Earth system modelling with a particular interest in the interactions of biogeochemical cycles with the climate system. Over the past years, I have been one of the main developers of the ocean biogeochemistry module of the Norwegian Earth System Model (NorESM). I am involved into the efforts of the Global Carbon Project to quantify the contemporary global to regional carbon sinks. More recently, I became also interested in assessing climate mitigation pathways and mitigation options. Given the huge mitigation challenges that have accumulated over the past decades, I am interested in assessing the feasibility of Carbon Dioxide Removal (CDR) through methods such as bio-energy combined with CCS or Ocean Alkalinity Enhancement among others. My contribution to such assessments is through a global perspective of an Earth system modeller with a focus on Earth system feedbacks and biogeochemical cycles.
Jörg Schwinger
Forsker II
jrsc@norceresearch.no
+47 56 10 75 51
Jahnebakken 5, 5007 Bergen, Norway
Divisjon
Klima og miljø
Forskningstema
Forskergrupper
Mer info om Jörg
Prosjekter
-
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
-
KonferanseforedragCE2COAST: Case Study 7: Norway.– Norkyst Working Group meeting 2024
-
Vitenskapelig artikkelOn the emission-path dependency of the efficiency of ocean alkalinity enhancement– Environmental Research Letters 2024
-
Vitenskapelig artikkelNet primary production annual maxima in the North Atlantic projected to shift in the 21st century– Biogeosciences 2024
-
Vitenskapelig artikkelSimulated Abrupt Shifts in Aerobic Habitats of Marine Species in the Past, Present, and Future– Earth's Future 2024
-
Vitenskapelig artikkelMore Frequent Abrupt Marine Environmental Changes Expected– Geophysical Research Letters 2024
-
Vitenskapelig artikkelA Synthesis of Global Coastal Ocean Greenhouse Gas Fluxes– Global Biogeochemical Cycles 2024
-
KonferanseforedragInfluence of AMOC decline and recovery on ZEC and TCRE– An assessment of TCRE and ZEC 2024
-
Vitenskapelig artikkelCarbon cycle feedbacks in an idealized simulation and a scenario simulation of negative emissions in CMIP6 Earth system models– Biogeosciences 2024
-
Vitenskapelig artikkelGlobal Carbon Budget 2023– Earth System Science Data 2023
-
KonferanseforedragRegional response of the Greenland ice sheet to overshoot scenarios– BCCR Regional Climate Information Mini-Workshop 2023
-
KonferanseforedragLessons from COVID-19 emission reduction simulations with NorESM2– CACTI (Composition Air quality Climate inTeractions Initiative) workshop 2023 2023
-
Vitenskapelig artikkelSimulations of ocean deoxygenation in the historical era: insights from forced and coupled models– Frontiers in Marine Science 2023
-
Vitenskapelig artikkelMagnitude, Trends, and Variability of the Global Ocean Carbon Sink From 1985 to 2018– Global Biogeochemical Cycles 2023
-
Vitenskapelig artikkelIrreversible loss in marine ecosystem habitability after a temperature overshoot– Communications Earth & Environment 2023
-
KonferanseforedragCarbon cycle feedbacks under negative emissions in CMIP6 Earth system models– Workshop on High-latitude Earth Climate System 2023
-
Vitenskapelig artikkelSeasonal Variability of the Surface Ocean Carbon Cycle: A Synthesis– Global Biogeochemical Cycles 2023
-
Vitenskapelig artikkelClimate-driven variability of the Southern Ocean CO2 sink– Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 2023
-
KonferanseforedragResponse of the Greenland Ice Sheet to temperature overshoot scenarios– Joint CESM Land Ice - Polar Climate Working Group meeting 2023
-
KonferanseforedragResponse of the Greenland Ice Sheet to temperature overshoot scenarios– Greenland Ice Sheet stability - Lessons from the past Workshop 2023
-
KonferanseforedragResponse of the Greenland Ice Sheet to temperature overshoot scenarios– EGU General Assembly 2023 2023
-
KonferanseforedragChanges in global fire regimes under idealized overshoot scenarios– EGU General Assembly 2023 2023
-
Vitenskapelig artikkelThe representation of alkalinity and the carbonate pump from CMIP5 to CMIP6 Earth system models and implications for the carbon cycle– Biogeosciences 2023
-
Vitenskapelig artikkelGlobal Surface Ocean Acidification Indicators From 1750 to 2100– Journal of Advances in Modeling Earth Systems 2023
-
KonferanseforedragConstraining ocean carbon sink projections in CMIP6 models– EGU 2023 2023
-
Vitenskapelig artikkelRiverine impact on future projections of marine primary production and carbon uptake– Biogeosciences 2023
-
KonferanseforedragCarbon cycle feedbacks in an idealized and a scenario simulation of carbon dioxide removal in CMIP6 Earth system models– EGU General Assembly 2022
-
KonferanseforedragConstraining the large spread in ocean carbon sinks in ESMs– ECMWF 6th WGNE workshop on systematic errors in weather and climate models 2022
-
Vitenskapelig artikkelEmit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations– Earth System Dynamics (ESD) 2022
-
Vitenskapelig artikkelGlobal Carbon Budget 2021– Earth System Science Data 2022
-
KonferanseforedragDetecting ecosystem-relevant crossings of thresholds– EGU General Assembly 2022 2022
-
Vitenskapelig artikkelHow Is the Ocean Anthropogenic Carbon Reservoir Filled?– Global Biogeochemical Cycles 2022
-
KonferanseforedragPossibility for strong northern hemisphere high-latitude cooling under zero and negative emissions– EGU General Assembly 2022
-
KonferanseforedragEmit now, mitigate later? Simulating the Earth system response to zero and negative emissions– Bjerknes Seminar 2022
-
Vitenskapelig artikkelPossibility for strong northern hemisphere high-latitude cooling under negative emissions– Nature Communications 2022
-
Vitenskapelig artikkelStratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S– Nature Communications 2022
-
KonferanseforedragEmit now, mitigate later? How can we meet the goals of the Paris Agreement?– NORCE Climate & Environment department seminar 2021 2021
-
KonferanseforedragPossibility of strong northern hemisphere high-latitude cooling under negative emissions– COMFORT virtual annual meeting 2021 2021
-
KonferanseforedragSkill assessment of a pan-Arctic downscaling ocean biogeochemical model (A20)– CE2COAST workshop M3.2 2021
-
Vitenskapelig artikkelImplications of temperature overshoot dynamics for climate and carbon dioxide removal policies in the DICE model– Environmental Research Letters 2021
-
Vitenskapelig artikkelEvaluation of ocean dimethylsulfide concentration and emission in CMIP6 models– Biogeosciences 2021
-
KonferanseforedragEfficient carbon drawdown allows for a high future carbon uptake in the North Atlantic– EGU General Assembly 2021 2021
-
Vitenskapelig artikkelCompatible fossil fuel CO2 emissions in the CMIP6 Earth system models’ historical and shared socioeconomic pathway experiments of the twenty-first century– Journal of Climate 2021
-
Vitenskapelig artikkelEvaluating the biological pump efficiency of the Last Glacial Maximum ocean using d13C– Climate of the Past 2021
-
Vitenskapelig artikkelThe response of terrestrial ecosystem carbon cycling under different aerosol-based radiation management geoengineering– Earth System Dynamics (ESD) 2021
-
Vitenskapelig artikkelOverview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations– Geoscientific Model Development 2020
-
Vitenskapelig artikkelGlobal Carbon Budget 2020– Earth System Science Data 2020
-
Vitenskapelig artikkelA Last Glacial Maximum forcing dataset for ocean modelling– Earth System Science Data 2020
-
Vitenskapelig artikkelConsistency and Challenges in the Ocean Carbon Sink Estimate for the Global Carbon Budget– Frontiers in Marine Science 2020
-
KonferanseforedragParis agreement, carbon budgets and negative emissions– NORCE Climate Science Day 2020
-
Vitenskapelig artikkelTracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6– Current Climate Change Reports 2020
-
Vitenskapelig artikkelCarbon–concentration and carbon–climate feedbacks in CMIP6 models and their comparison to CMIP5 models– Biogeosciences 2020
-
Vitenskapelig artikkelTwenty-first century ocean warming, acidification, deoxygenation, and upper-ocean nutrient and primary production decline from CMIP6 model projections– Biogeosciences 2020
-
Vitenskapelig artikkelIs there warming in the pipeline? A multi-model analysis of the Zero Emissions Commitment from CO2– Biogeosciences 2020
-
Vitenskapelig artikkelOcean biogeochemistry in the Norwegian Earth System Model version 2 (NorESM2)– Geoscientific Model Development 2020
-
KonferanseforedragOn the Potential of the Southern Ocean Biological Pump to Maintain the Ocean Carbon Sink under Negative Emissions– Ocean Sciences 2020 2020
-
KonferanseforedragStrength and reversibility of the ocean carbon sink under negative emissions– EGU 2020 2020
-
Vitenskapelig oversiktsartikkelThe impacts of ocean acidification on marine trace gases and the implications for atmospheric chemistry and climate– Proceedings of the Royal Society. Mathematical, Physical and Engineering Sciences 2020
-
Vitenskapelig artikkelGlobal carbon budget 2019– Earth System Science Data 2019
-
Vitenskapelig artikkelDecadal trends in the ocean carbon sink– Proceedings of the National Academy of Sciences of the United States of America (PNAS) 2019