Ocean-Atmosphere CO2 Exchange - Climate Model: SSP5 (Fossil-fueled Development) - 2015 - 2100
DetailsPermalink to Details
- Added to the Catalog
- Available for
- People: Human Impact
- Water: Human Impact, Chemistry
- Anthropogenic Emissions
- Carbon Cycle
- Carbon Dioxide
- Carbon Flux
- Climate Models
- Ocean Acidificaiton
- Ocean Climate
DescriptionPermalink to Description
What are Climate Models?Permalink to What are Climate Models?
Climate and Earth system models are used for a variety of purposes - from the study of dynamics of the weather and climate system of the past to projecting future climate. These models simulate the physics, chemistry and biology of the atmosphere, land and oceans, and require massive supercomputers to generate climate projections.
An international team of climate scientists, economists and earth systems modelers have built a range of new "pathways" that examine how global society, demographics and economics might change over the next century. They are collectively known as the "Shared Socioeconomic Pathways" (SSPs). World Climate Research Programme climate modeling working group, through international science coordination and partnerships, designed the framework for these climate models to inform the Intergovernmental Panel on Climate Change Sixth Assessment Report, AR6.
NOAA's Geophysical Fluid Dynamics Laboratory (GFDL) has created several fully coupled climate and earth system models that can utilize the SSPs to glimpse into the future. Global climate models represent the planet as millions of grid boxes and then solve mathematical equations to calculate how energy is transferred between those boxes using the laws of thermodynamics. If done correctly, these models of how energy is cycled through all parts of the planet can be used to estimate dozens of environmental variables (winds, temperature, moisture, ocean acidification, etc.). The models are tested by simulating historical conditions and then matching the results to our historical observational records. If the models can adequately recreate the past, they are then run forward in time to project what may happen in the future.
What is the Ocean-Atmosphere CO2 Exchange?Permalink to What is the Ocean-Atmosphere CO2 Exchange?
In this dataset, the ocean-atmosphere exchange of carbon dioxide is shown as projected by the SSP5 scenario, using GFDL’s ESM4 model between 2015 and 2100. SSP5-8.5 is a very high greenhouse gas emissions scenario - and unlikely to happen - where carbon dioxide emissions triple by 2075. The resolution of the climate model is 1/4 degree for the oceans and 1 degree for the atmosphere.
When carbon dioxide, CO2, is released into the atmosphere from the burning of fossil fuels, approximately 50% remains in the atmosphere, while 25% is absorbed by land plants and trees, and the other 25% is absorbed into certain areas of the ocean. In other areas of the ocean, where the concentration of CO2 is higher in the water than in the atmosphere above, CO2 is released to the atmosphere.
This transfer of CO2 out of the ocean to the atmosphere is referred to as a positive "flux" while a negative flux means that the ocean is absorbing CO2. The ocean has a complicated pattern of both positive and negative fluxes. Prior to the Industrial Revolution and the burning of fossil fuels, the net global ocean flux was slightly positive to offset the absorption of CO2 by land plants. Today, humans have reversed that trend so the oceans absorb more CO2 than they release although the complicated pattern of positive and negative fluxes still exists.
Regions of upwelling (the equatorial Pacific and the west coast of South America) are natural sources of CO2, where old water with high concentrations of CO2 is brought to the surface, and the excess CO2 is degassed into the atmosphere. Colder regions are capable of absorbing more CO2 than warm regions, so the polar regions tend to be sinks of CO2 (see the North Atlantic and Arctic). As atmospheric CO2 increases from the burning of fossil fuels, more regions of the ocean absorb CO2 from the atmosphere, and the global ocean source and sink regions are no longer in balance. By 2100, much of the global ocean is expected to be a sink of CO2 from the atmosphere. As this CO2 dissolves into the ocean, it alters the ocean chemistry and lowers the pH of the water.
For more information on understanding SSPs we found this carbonbrief.org article very informative.
SSP Narratives for each Emission ScenarioPermalink to SSP Narratives for each Emission Scenario
(Note: OnlySSP1, SSP2 and SSP5 are available on SOS)
SSP1 Sustainability – Taking the Green Road (Low challenges to mitigation and adaptation)Permalink to SSP1 Sustainability – Taking the Green Road (Low challenges to mitigation and adaptation)
The world shifts gradually, but pervasively, toward a more sustainable path, emphasizing more inclusive development that respects perceived environmental boundaries. Management of the global commons slowly improves, educational and health investments accelerate the demographic transition, and the emphasis on economic growth shifts toward a broader emphasis on human well-being. Driven by an increasing commitment to achieving development goals, inequality is reduced both across and within countries. Consumption is oriented toward low material growth and lower resource and energy intensity.
SSP2 Middle of the Road (Medium challenges to mitigation and adaptation)Permalink to SSP2 Middle of the Road (Medium challenges to mitigation and adaptation)
The world follows a path in which social, economic, and technological trends do not shift markedly from historical patterns. Development and income growth proceeds unevenly, with some countries making relatively good progress while others fall short of expectations. Global and national institutions work toward but make slow progress in achieving sustainable development goals. Environmental systems experience degradation, although there are some improvements and overall the intensity of resource and energy use declines. Global population growth is moderate and levels off in the second half of the century. Income inequality persists or improves only slowly and challenges to reducing vulnerability to societal and environmental changes remain.
SSP3 Regional Rivalry – A Rocky Road (High challenges to mitigation and adaptation)Permalink to SSP3 Regional Rivalry – A Rocky Road (High challenges to mitigation and adaptation)
A resurgent nationalism, concerns about competitiveness and security, and regional conflicts push countries to increasingly focus on domestic or, at most, regional issues. Policies shift over time to become increasingly oriented toward national and regional security issues. Countries focus on achieving energy and food security goals within their own regions at the expense of broader-based development. Investments in education and technological development decline. Economic development is slow, consumption is material-intensive, and inequalities persist or worsen over time. Population growth is low in industrialized and high in developing countries. A low international priority for addressing environmental concerns leads to strong environmental degradation in some regions.
SSP4 Inequality – A Road Divided (Low challenges to mitigation, high challenges to adaptation)Permalink to SSP4 Inequality – A Road Divided (Low challenges to mitigation, high challenges to adaptation)
Highly unequal investments in human capital, combined with increasing disparities in economic opportunity and political power, lead to increasing inequalities and stratification both across and within countries. Over time, a gap widens between an internationally-connected society that contributes to knowledge- and capital-intensive sectors of the global economy, and a fragmented collection of lower-income, poorly educated societies that work in a labor intensive, low-tech economy. Social cohesion degrades and conflict and unrest become increasingly common. Technology development is high in the high-tech economy and sectors. The globally connected energy sector diversifies, with investments in both carbon-intensive fuels like coal and unconventional oil, but also low-carbon energy sources. Environmental policies focus on local issues around middle and high income areas.
SSP5 Fossil-fueled Development – Taking the Highway (High challenges to mitigation, low challenges to adaptation)Permalink to SSP5 Fossil-fueled Development – Taking the Highway (High challenges to mitigation, low challenges to adaptation)
This world places increasing faith in competitive markets, innovation and participatory societies to produce rapid technological progress and development of human capital as the path to sustainable development. Global markets are increasingly integrated. There are also strong investments in health, education, and institutions to enhance human and social capital. At the same time, the push for economic and social development is coupled with the exploitation of abundant fossil fuel resources and the adoption of resource and energy intensive lifestyles around the world. All these factors lead to rapid growth of the global economy, while global population peaks and declines in the 21st century. Local environmental problems like air pollution are successfully managed. There is faith in the ability to effectively manage social and ecological systems, including by geo-engineering if necessary.
Narratives for each Shared Socioeconomic Pathway, from Riahi et al 2017.
Suggested Educational MaterialsPermalink to Suggested Educational Materials
- Climate Literacy and Energy Awareness Network (CLEAN): Teaching Climate and Energy - Principle 5
- Climate Interactives - Climate Change Solutions Simulators
- Climate Literacy and Energy Awareness Network (CLEAN): Webinar Series
- Climate Literacy and Energy Awareness Network (CLEAN): Climate Model Resource Collection
- Data Puzzles - CIRES Education and Outreach
- Antarctica: Connecting Climate Change, Melting Ice Shelves, and Pooping Penguins - CIRES Education and Outreach Arctic Feedbacks - Not All Warming Is Equal - CIRES Education and Outreach
- Climate and Resiliency Education - CIRES Education and Outreach
For more technical information on the World Climate Research Programme go to the Earth System Grid Federation.
References:Permalink to References:
- Dunne, J. P., Horowitz, L. W., Adcroft, A. J., Ginoux, P., Held, I. M., John, J. G., ... & Zhao, M. (2020). The GFDL Earth System Model version 4.1 (GFDL‐ESM 4.1): Overall coupled model description and simulation characteristics. Journal of Advances in Modeling Earth Systems, 12(11), e2019MS002015.
- O’Neill, B. C., et al., The roads ahead: Narratives for shared socioeconomic pathways describing world futures in the 21st century, Global Environ. Change (2015), .
- O'Neill, B. C., et al., The Scenario Model IntercomparisonProject (ScenarioMIP) for CMIP6,Geosci. Model Dev., 9, 3461-3482, doi:10.5194/gmd-9-3461-2016, 2016.
- Riahi, K. et al., The Shared Socioeconomic Pathways and their energy, land use, and greenhouse gas emissions implications: An overview, Global Environmental Change, Volume 42, 2017, Pages 153-168,
Notable FeaturesPermalink to Notable Features
- When carbon dioxide CO2 is released into the atmosphere from the burning of fossil fuels, approximately 50% remains in the atmosphere, while 25% is absorbed by land plants and trees, and the other 25% is absorbed into certain areas of the ocean
- The transfer of CO2 out of the ocean to the atmosphere is referred to as a positive "flux" while a negative flux means that the ocean is absorbing CO2
- As atmospheric CO2 increases from the burning of fossil fuels, more regions of the ocean absorb CO2 from the atmosphere
- This dataset shows projected changes in the Fossil-fueled Development - SSP5 future scenario, a very high emissions scenario where carbon dioxide emissions triple by 2075
Data SourcePermalink to Data Source
World Climate Research Programme CMIP6World Climate Research Programme CMIP6