SURFER v2.0: a flexible and simple model linking anthropogenic CO2 emissions and solar radiation modification to ocean acidification and sea level rise
Abstract:Abstract. We present SURFER, a novel reduced model for estimating the impact of CO2 emissions and solar radiation modification options on sea level rise and ocean acidification over timescales of several thousands of years.
SURFER has been designed for the analysis of CO2 emission and solar radiation modification policies, for supporting the computation of optimal (CO2 emission and solar radiation modification) policies and for the study of commitment and responsibility under uncertainty.
The model is based on… Show more
“…Two recent comprehensive model intercomparison projects have been dedicated to identify how the Earth system reacts if greenhouse gas emissions are set to zero at a certain point in time (ZECMIP, Zero Emissions Commitment Intercomparison 435 Project) (Jones et al, 2019), and how it reacts if additionally negative CO2 emissions can be achieved (CDRMIP, Carbon Dioxide Removal Model Intercomparison Project) (Keller et al, 2018). The first ZECMIP results confirm that the abrupt global surface air temperature rise since the start of industrialisation is only slowly -if at all -attenuated over time even if greenhouse gas emissions swiftly go to zero (Montero et al, 2022;Schwinger et al, 2022b). The picture changes for massive carbon dioxide removals from the atmosphere, where the global mean surface air temperature approaches the preindustrial 440 levels if indeed preindustrial CO2 concentrations were re-established (Jeltsch-Thömmes et al, 2020;.…”
Section: Abrupt Global Changes In Warmingmentioning
Abstract. Abrupt changes in ocean biogeochemical variables occur as a result of human-induced climate forcing as well as those which are more gradual and occur over longer timescales. These abrupt changes have not yet been identified and quantified to the same extent as the more gradual ones. We review and synthesise abrupt changes in ocean biogeochemistry under human-induced climatic forcing. We specifically address the ocean carbon and oxygen cycles because the related processes of acidification and deoxygenation provide important ecosystem hazards. Since biogeochemical cycles depend also on the physical environment, we also describe the relevant changes in warming, circulation, and sea ice. We include an overview of the reversibility or irreversibility of abrupt marine biogeochemical changes. Important implications of abrupt biogeochemical changes for ecosystems are also discussed. We conclude that there is evidence for increasing occurrence and extent of abrupt changes in ocean biogeochemistry as a consequence of rising greenhouse gas emissions.
“…Two recent comprehensive model intercomparison projects have been dedicated to identify how the Earth system reacts if greenhouse gas emissions are set to zero at a certain point in time (ZECMIP, Zero Emissions Commitment Intercomparison 435 Project) (Jones et al, 2019), and how it reacts if additionally negative CO2 emissions can be achieved (CDRMIP, Carbon Dioxide Removal Model Intercomparison Project) (Keller et al, 2018). The first ZECMIP results confirm that the abrupt global surface air temperature rise since the start of industrialisation is only slowly -if at all -attenuated over time even if greenhouse gas emissions swiftly go to zero (Montero et al, 2022;Schwinger et al, 2022b). The picture changes for massive carbon dioxide removals from the atmosphere, where the global mean surface air temperature approaches the preindustrial 440 levels if indeed preindustrial CO2 concentrations were re-established (Jeltsch-Thömmes et al, 2020;.…”
Section: Abrupt Global Changes In Warmingmentioning
Abstract. Abrupt changes in ocean biogeochemical variables occur as a result of human-induced climate forcing as well as those which are more gradual and occur over longer timescales. These abrupt changes have not yet been identified and quantified to the same extent as the more gradual ones. We review and synthesise abrupt changes in ocean biogeochemistry under human-induced climatic forcing. We specifically address the ocean carbon and oxygen cycles because the related processes of acidification and deoxygenation provide important ecosystem hazards. Since biogeochemical cycles depend also on the physical environment, we also describe the relevant changes in warming, circulation, and sea ice. We include an overview of the reversibility or irreversibility of abrupt marine biogeochemical changes. Important implications of abrupt biogeochemical changes for ecosystems are also discussed. We conclude that there is evidence for increasing occurrence and extent of abrupt changes in ocean biogeochemistry as a consequence of rising greenhouse gas emissions.
“…Breakdown of Model Suitability by Complexity. References[2,[78][79][80][81][82][83][84][85][86][87][88][89][129][130][131][132][133][134][135][136][137][138][181][182][183][184][185][186][187][188] are cited in the supplementary materials.Author Contributions: Conceptualization, X.Y. and B.C.…”
Understanding the oceanic carbon cycle, particularly in the Arctic regions, is crucial for addressing climate change. However, significant research gaps persist, especially regarding climate effects on the oceanic carbon cycle in these regions. This review systematically explores Arctic-related research, focusing on mechanisms, regulatory frameworks, and modelling approaches in the oceanic carbon cycle, carbon sink, climate change impact, and maritime shipping. The findings highlight the Arctic’s limited observer presence and high operational costs, hindering the data availability and studies on carbon-cycle changes. This underscores the need to integrate real-time Arctic Ocean monitoring data. Carbon sink research urgently requires direct methods to measure anthropogenic carbon uptake and address uncertainties in air–ocean carbon fluxes due to sea ice melting. Unlike terrestrial carbon cycling research, carbon-cycle studies in the oceans, which are essential for absorbing anthropogenic emissions, receive insufficient attention, especially in the Arctic regions. Numerous policies often fall short in achieving effective mitigation, frequently depending on voluntary or market-based approaches. Analyzing carbon-cycle and sink models has uncovered limitations, primarily due to their global perspective, hampering in-depth assessments of climate change effects on the Arctic regions. To pave the way for future research, enhancing Arctic Ocean climate data availability is recommended, as well as fostering international cooperation in carbon-cycle research, enforcing carbon policies, and improving regional modelling in the Arctic Ocean.
We propose to explore the sustainability of climate policies based on a novel commitment metric. This metric allows to quantify how future generations’ scope of action is affected by short-term climate policy. In an example application, we show that following a moderate emission scenario like SSP2-4.5 will commit future generations to heavily rely on carbon dioxide removal or/and solar radiation modification to avoid unmanageable sea level rise.
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