Jeg er en kjemisk oseanograf av bakgrunn og forskningen min fokuserer på analyse av karbonkretsløpet i havet. Jeg fokuserer spesielt på endringer som er skjedd de siste ti-årene, men også årsakene til, og mekanismene bak, disse endringene. Jeg ønsker å øke forståelsen av karbonkretsløpet i havet, både når det kommer til naturlig variabilitet og antropogene endringer, inkludert hvordan disse endringene vil utvikle seg i fremtiden. Jeg bruker mange verktøy i forskningen min, både observasjonelle og modellbaserte. Det er veldig viktig å ha robuste observasjonsdata av høy kvalitet for å kunne svare på disse viktige spørsmålene om planetens karbonkretsløp og jeg er derfor engasjert i flere internasjonale forskningsinfrastrukturer. Fremst av dem er Integrated Carbon Observing System (ICOS) hvor jeg koordinerer den norske greina: ICOS Norge og OTC, et prosjekt finansiert av Norges Forskningsråd.
Siv Kari Lauvset
Forsker II
sivk@norceresearch.no
+47 56 10 75 33
Jahnebakken 5, 5007 Bergen, Norway
Divisjon
Klima og miljø
Forskningstema
Forskergrupper
Mer info om Siv
Last ned pressebildeKilde: Universitetet i Bergen
Prosjekter
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Vitenskapelig artikkelIn the Wake of Deeper Convection: Nonsteady State Anthropogenic Carbon in the Greenland Sea– Journal of Geophysical Research (JGR): Oceans 2024
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Vitenskapelig artikkelSynthesis Product for Ocean Time Series (SPOTS) - a ship-based biogeochemical pilot– Earth System Science Data 2024
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Vitenskapelig artikkelAdvances in understanding of air-sea exchange and cycling of greenhouse gases in the upper ocean– Elementa: Science of the Anthropocene 2024
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FagartikkelStorylines: physical impacts– zenodo 2023
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Vitenskapelig artikkelSynthesis Product for Ocean Time-Series (SPOTS) – A ship-based biogeochemical pilot– Hydrology and Earth System Sciences Discussions (HESSD) 2023
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KonferanseforedragDecadal trends from the Ocean Weather Station M– Bjerknes Annual Meeting 2023
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KonferanseforedragDecadal trends from the Ocean Weather Station M– ICOS Nordic Conference 2023
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Vitenskapelig artikkelDecadal Trends in the Oceanic Storage of Anthropogenic Carbon From 1994 to 2014– AGU Advances 2023
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Vitenskapelig artikkelOn the Origins of Open Ocean Oxygen Minimum Zones– Journal of Geophysical Research (JGR): Oceans 2023
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Vitenskapelig artikkelRespiration Patterns in the Dark Ocean– Global Biogeochemical Cycles 2023
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Vitenskapelig artikkelContext matters when using climate model projections for aquaculture– Frontiers in Marine Science 2023
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Vitenskapelig artikkelA status assessment of selected data synthesis products for ocean biogeochemistry– Frontiers in Marine Science 2023
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Vitenskapelig artikkelRecent Trends and Variability in the Oceanic Storage of Dissolved Inorganic Carbon– Global Biogeochemical Cycles 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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KonferanseforedragClimate and Humans– Forelesning i Urban Sustainable Architechture 2023
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KonferanseforedragAnthropogenic ocean acidification below the surface: does organic matter cycling result in enhanced vulnerability?– Ocean Sciences Meeting 2022 2022
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Vitenskapelig artikkelGLODAPv2.2022: the latest version of the global interior ocean biogeochemical data product– Earth System Science Data 2022
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Vitenskapelig artikkelObservation-based Sea surface temperature trends in Atlantic large marine ecosystems– Progress in Oceanography 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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Vitenskapelig artikkelGlobal Carbon Budget 2021– Earth System Science Data 2022
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Vitenskapelig artikkelDecadal trends in Ocean Acidification from the Ocean Weather Station M in the Norwegian Sea– Journal of Marine Systems 2022
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Vitenskapelig artikkelHow Is the Ocean Anthropogenic Carbon Reservoir Filled?– Global Biogeochemical Cycles 2022
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Vitenskapelig artikkelBest Practice Data Standards for Discrete Chemical Oceanographic Observations– Frontiers in Marine Science 2022
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Vitenskapelig artikkelAcidification of the Nordic Seas– Biogeosciences 2022
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Vitenskapelig oversiktsartikkelNordic Seas Heat Loss, Atlantic Inflow, and Arctic Sea Ice cover over the last century– Reviews of Geophysics 2022
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KonferanseforedragSurface ocean CO2 in the northern North Sea - temporal and spatial variability– ICOS Nordic 2021
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KonferanseforedragTemporal and spatial variability of CO2 in the northern North Sea– ICOS Norge 2021
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AviskronikkHvordan skal vi følge med på CO2 utslippene?– Klassekampen 2021
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KonferanseforedragAnthropogenic ocean acidification below the surface: does organic matter cycling result in enhanced vulnerability?– vEGU21 2021
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FagartikkelA vision for FAIR ocean data products– Communications Earth & Environment 2021
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Vitenskapelig artikkelAn updated version of the global interior ocean biogeochemical data product, GLODAPv2.2021– Earth System Science Data 2021
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Vitenskapelig artikkelCalcium carbonate dissolution patterns in the ocean– Nature Geoscience 2021
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Vitenskapelig oversiktsartikkelA Global Ocean Oxygen Database and Atlas for Assessing and Predicting Deoxygenation and Ocean Health in the Open and Coastal Ocean– Frontiers in Marine Science 2021
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ForskningsrapportIntegrated Ocean Carbon Research: A Summary of Ocean Carbon Research, and Vision of Coordinated Ocean Carbon Research and Observations for the Next Decade. [R. Wanninkhof, C. Sabine and S. Aricò (eds.)]– UNESCO, (IOC Technical Series, 158.) doi:10.25607/h0gj-pq41 2021
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KonferanseforedragEfficient carbon drawdown allows for a high future carbon uptake in the North Atlantic– EGU General Assembly 2021 2021
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Vitenskapelig artikkelPreformed properties for marine organic matter and carbonate mineral cycling quantification– Global Biogeochemical Cycles 2021
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ForskningsrapportMonitoring ocean acidification in Norwegian seas in 2019– Miljødirektoratet 2020
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Vitenskapelig artikkelDissolved inorganic nutrients in the western Mediterranean Sea (2004–2017)– Earth System Science Data 2020
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Vitenskapelig artikkelCurrent estimates of K1* and K2* appear inconsistent with measured CO2 system parameters in cold oceanic regions.– Ocean Science Journal 2020
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Vitenskapelig artikkelAn updated version of the global interior ocean biogeochemical data product, GLODAPv2.2020– Earth System Science Data 2020
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Vitenskapelig artikkelSeasonal Carbon Dynamics in the Near-Global Ocean– Global Biogeochemical Cycles 2020
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Vitenskapelig artikkelProcesses Driving Global Interior Ocean pH Distribution– Global Biogeochemical Cycles 2020
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Vitenskapelig artikkelWinter weather controls net influx of atmospheric CO2 on the north-west European shelf– Scientific Reports 2019
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Vitenskapelig artikkelGlobal carbon budget 2019– Earth System Science Data 2019
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Vitenskapelig artikkelSurface ocean pH and buffer capacity: past, present and future– Scientific Reports 2019
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Vitenskapelig artikkelGLODAPv2.2019-an update of GLODAPv2– Earth System Science Data 2019
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Vitenskapelig artikkelThe oceanic sink for anthropogenic CO2 from 1994 to 2007– Science 2019
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Vitenskapelig artikkelSudden emergence of a shallow aragonite saturation horizon in the Southern Ocean– Nature Climate Change 2019
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Vitenskapelig artikkelReconciling Observation and Model Trends in North Atlantic Surface CO2– Global Biogeochemical Cycles 2019
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Populærvitenskapelig artikkelKarbonkretsløpet– 2grader C 2019
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KonferanseforedragThe Carbon Cycle: The role of oceans and humans– SOLAS Open Science Conference 2019
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Vitenskapelig oversiktsartikkelConstraining the oceanic uptake and fluxes of greenhouse gases by building an ocean network of certified stations: The ocean component of the Integrated Carbon Observation System, ICOS-Oceans– Frontiers in Marine Science 2019
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Vitenskapelig oversiktsartikkelA surface ocean CO2 reference network, SOCONET and associated marine boundary layer CO2 measurements– Frontiers in Marine Science 2019
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KonferanseforedragObservations-constrained projections reveal early and strong deoxygenation in the interior North Atlantic– AGU Annual meeting 2018 2018
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Populærvitenskapelig artikkelEn misforståelse oppklart – med Non Stop– Energi og Klima : Norsk klimastiftelses nettmagasin 2018
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KonferanseforedragOn the Spatial Variability of Ocean pH and its Primary Drivers– Ocean Sciences Meeting 2018 2018
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KonferanseforedragCoastal carbon data at a range of frequencies– Observational and modeling capabilities of coastal biogeochemistry and ecosystems 2018
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Vitenskapelig artikkelContinued warming, salinification and oxygenation of the Greenland Sea gyre– Tellus A: Dynamic Meteorology and Oceanography 2018
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KonferanseforedragEarly detection of anthropogenic climate change signal in the interior subpolar North Atlantic– Ocean Deoxygenation Conference 2018
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Vitenskapelig artikkelArctic Ocean CO2 uptake: An improved multiyear estimate of the air-sea CO2 flux incorporating chlorophyll a concentrations– Biogeosciences 2018
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Vitenskapelig artikkelMechanisms and early detections of multidecadal oxygen changes in the interior subpolar North Atlantic– Geophysical Research Letters 2018
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KonferanseforedragEarly detection of anthropogenic climate change signal in the interior subpolar North Atlantic oxygen– 50th International Liege Colloquium on Ocean Dynamics 2018
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Vitenskapelig artikkelConstraining Projection-Based Estimates of the Future North Atlantic Carbon Uptake– Journal of Climate 2018
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Vitenskapelig artikkelClimate response to aerosol geoengineering: a multi-method comparison– Journal of Climate 2018
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Vitenskapelig artikkelInorganic Carbon and Water Masses in the Irminger Sea since 1991– Biogeosciences 2018
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Vitenskapelig artikkelCan Empirical Algorithms Successfully Estimate Aragonite Saturation State in the Subpolar North Atlantic?– Frontiers in Marine Science 2017
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ForskningsrapportHavforsuringsovervåking i norske farvann i 2016– Miljødirektoratet 2017