Short Answer

Both the model and the market expect CO2 atmospheric concentration to reach at least 440 before 2030, with no compelling evidence of mispricing.

1. Executive Verdict

  • Global fossil fuel capacity, especially coal, is projected to increase through 2028.
  • Increased fossil fuel use directly drives higher atmospheric CO2 emissions.
  • Atmospheric methane concentrations are accelerating, reaching record-high growth rates.
  • El Niño events significantly increase the annual atmospheric CO2 growth rate.

Who Wins and Why

Outcome Market Model Why
At least 450 22.0% 21.9% Increasing global fossil fuel capacity and accelerating methane levels drive higher CO2 concentrations.
At least 440 93.0% 91.9% Increasing global fossil fuel capacity and accelerating methane levels drive higher CO2 concentrations.
At least 460 3.0% 3.2% Increasing global fossil fuel capacity and accelerating methane levels drive higher CO2 concentrations.
At least 445 38.0% 36.6% Increasing global fossil fuel capacity and accelerating methane levels drive higher CO2 concentrations.
At least 455 13.0% 13.4% Increasing global fossil fuel capacity and accelerating methane levels drive higher CO2 concentrations.

2. Market Behavior & Price Dynamics

Historical Price (Probability)

Outcome probability
Date
Based on the chart data, this market exhibits a highly stable and sideways price trend, indicating a strong consensus. The price has been confined to an extremely narrow one-percentage-point range, moving from a starting probability of 92.0% to its current level of 93.0%. There have been no significant price spikes, drops, or periods of volatility throughout the market's history. The lack of price movement means there are no events to correlate with the provided context. Overall, the chart reflects a persistent and unwavering market sentiment that a "YES" resolution is overwhelmingly likely.
The most critical feature of this market is the exceptionally low trading volume, with a total of only one contract traded. The price has shifted despite periods of zero volume, which suggests adjustments in orders rather than active trading between participants. This extremely low liquidity indicates a lack of broad market engagement or conviction. While the price is very high, the minimal volume suggests this high probability is determined by a very small number of participants and may not reflect a wider market opinion. The 92.0% and 93.0% levels have acted as the effective support and resistance for the market's entire duration.

3. Significant Price Movements

Notable price changes detected in the chart, along with research into what caused each movement.

📉 April 25, 2026: 10.0pp drop

Price decreased from 24.0% to 14.0%

Outcome: At least 450

What happened: No supporting research available for this anomaly.

4. Market Data

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Contract Snapshot

This market resolves to "Yes" if the atmospheric concentration of CO2 reaches at least 445 before January 2030; otherwise, it resolves to "No." The outcome is verified using data from the National Aeronautics and Space Administration (NASA) and NOAA Global Monitoring Laboratory. The market will close early if the specified CO2 level is reached, or by December 31, 2029, at 11:59 pm EST if the event does not occur.

Available Contracts

Market options and current pricing

Outcome bucket Yes (price) No (price) Last trade probability
At least 440 $0.93 $0.16 93%
At least 445 $0.44 $0.62 38%
At least 450 $0.23 $0.86 22%
At least 455 $0.13 $0.94 13%
At least 460 $0.08 $0.97 3%

Market Discussion

Traders are primarily discussing the probability of CO2 atmospheric concentration reaching at least 445 ppm by 2030. Arguments against reaching 445 ppm cite NOAA's prediction of 437 ppm and suggest that 445 ppm would require an improbable doubling of global CO2 emissions from current levels. While the market currently prices a 38% chance of reaching 445 ppm, the visible discussion posts strongly lean towards a "No" outcome, with traders calling it "easy money" due to the perceived unlikelihood based on current models and emission trends.

5. How Will Global Fossil Fuel Capacity Change by 2028?

India Thermal Capacity Under ConstructionApproximately 39.5 GW [^]
Global Coal Power Capacity Net ChangeProjected net increase [^]
US Coal Capacity TrendContinued retirements projected [^]
Global fossil fuel capacity projects a net increase in coal power. A net increase in overall coal power generation capacity is projected globally through 2028, primarily driven by new plant construction in Asia, which currently outpaces retirements in other regions [^]. India, for example, has approximately 39.5 GW of thermal capacity under construction, much of which is coal-fired [^]. While China remains a significant contributor to new builds, despite potentially slowing additions, the International Energy Agency (IEA) suggests that fossil fuel's overall share of global electricity generation will decline as renewables expand, according to the "World Energy Outlook 2025" [^].
United States' fossil fuel trends differ, with coal retirements continuing. In the United States, the U.S. Energy Information Administration (EIA) projects ongoing retirements of coal-fired generating capacity [^]. However, the EIA also notes that some scheduled retirements of U.S. electric generating capacity, including fossil fuel plants, may be delayed, potentially keeping existing capacity online longer than initially planned [^]. Natural gas-fired capacity is expected to remain a major part of the U.S. electricity mix, balancing retirements and providing flexible generation [^]. Globally, oil-fired generation is not projected for significant new large-scale power generation, serving primarily niche or backup roles [^].

6. What Are Projected Deforestation Trends in Amazon and Congo Basins?

Amazon Deforestation Reduction56-56.4% in January 2026 [^]
Brazil Amazon ProjectionLowest annual rate on record [^]
Congo Basin StatusForest loss requires immediate action [^]
Amazon Basin deforestation is projected to significantly decrease, reaching record lows. Brazil's Instituto Nacional de Pesquisas Espaciais (INPE) indicates a substantial reduction, with deforestation falling by 56% to 56.4% in January 2026 [^]. The Brazilian government anticipates that Amazon deforestation will be the lowest on record [^]. This positive trajectory is further corroborated by data from PRODES and BiomasBR, consistently showing a reduction in deforestation across the Brazilian Amazon [^].
The Congo Basin faces persistent forest loss, impacting carbon sequestration capacity. Conversely, the Congo Basin continues to experience forest loss trends that necessitate immediate intervention [^]. While specific future percentage projections for deforestation rates in the Congo Basin are not available, the emphasis on ongoing loss signals a sustained negative impact [^]. Both Amazonian and African tropical forests are simultaneously experiencing asynchronous carbon sink saturation, meaning their ability to absorb atmospheric carbon dioxide is diminishing [^]. Although deforestation directly hinders carbon sequestration, the provided research does not quantify a specific projected annual loss in gigatons of carbon directly linked to these future deforestation trends.

7. How Do El Niño Events Affect CO2 and Future Forecasts?

El Niño's Impact on CO2 GrowthIncreased annual rate of atmospheric CO2 concentration growth [^]
Primary Driver of CO2 IncreaseReduced terrestrial productivity, especially in tropical regions [^]
El Niño Long-Range Forecasts (Pre-2030)Not available years in advance for specific timing/intensity from NOAA/ECMWF [^]
El Niño significantly increases the annual atmospheric CO2 growth rate. Climate model sensitivity analyses indicate that El Niño events notably boost the annual rate of atmospheric CO2 increase [^]. This phenomenon is largely attributed to reduced terrestrial productivity, especially in tropical ecosystems, thereby diminishing Earth's natural capacity to absorb CO2 [^]. While the relationship is complex and involves compensatory effects, the general trend of increased CO2 growth during El Niño is consistently observed across various analyses [^]. Observations following the 2023/24 El Niño are also anticipated to show an increased CO2 growth rate in a warming climate [^].
No specific long-range El Niño forecasts exist before 2030. Neither the U.S. National Oceanic and Atmospheric Administration (NOAA) nor the European Centre for Medium-Range Weather Forecasts (ECMWF) provides specific predictions for the timing or intensity of individual El Niño events years in advance. Current seasonal forecasting methodologies typically offer outlooks for the next 6 to 12 months [^]. For example, NOAA's Climate Prediction Center issues regular ENSO Diagnostic Discussions and probability forecasts focused on the likelihood of conditions for upcoming seasons [^]. Similarly, ECMWF's seasonal forecasts generally extend up to six months ahead; while models accurately predicted the 2023/24 El Niño, forecasting the precise timing and strength of future events years into the future remains a significant challenge [^]. Therefore, no definitive long-range forecasts for El Niño occurrences before 2030 from these agencies are currently available.

8. What Are the Latest Trends in Atmospheric Methane Levels?

Atmospheric Methane 20231922.6 ppb [^]
Annual Methane Increase 202310.8 ppb [^]
Tropical Wetland Contribution30-40% of global emissions [^]
Atmospheric methane concentrations are accelerating, with recent record-high growth rates. Globally, the average atmospheric methane reached 1922.6 ppb in 2023 [^]. While the annual increase of 10.8 ppb in 2023 was slightly lower than in 2022 and 2021, these figures remain among the highest recorded since the 1980s [^]. Notably, the period between 2020 and 2022 experienced record-high growth rates [^]. Overall, atmospheric methane has been steadily rising since 2007, with isotopic analyses indicating microbial emissions from sources such as wetlands, agriculture, and waste as primary drivers [^].
Tropical wetlands are the largest natural methane source, increasing emissions. These wetlands contribute 30-40% of total global methane emissions and approximately 79% of all natural wetland emissions [^]. From 2000 to 2017, global natural wetland methane emissions increased by 2.2% per year, with significant growth observed after 2007 [^]. As global temperatures rise, increased microbial activity within these wetlands is projected to lead to higher methane releases, thereby creating a positive feedback loop that could intensify climate change [^].
Arctic regions show increasing methane emissions, especially from thawing permafrost. These areas, including permafrost zones, are experiencing increasing methane emissions, with widespread releases occurring even during cold seasons [^]. The thawing of permafrost due to warming temperatures is particularly concerning, as it can release vast quantities of previously frozen organic carbon as methane, initiating another significant positive feedback loop [^]. Satellite data, such as from the Copernicus Sentinel-5P, assists in monitoring these Arctic-boreal methane emissions, yet current models often underestimate these releases, especially during shoulder seasons and winter [^].

9. How Does Mauna Loa CO2 Data Authority Affect Markets?

Final Data AuthorityMauna Loa CO2 dataset by NOAA GML and Scripps [^]
Initial Data StatusPreliminary, subject to review and revision [^]
Historical Data RevisionsContinuously adjusted for quality assurance [^]
The Mauna Loa CO2 dataset serves as the definitive authority for CO2 prediction markets. This dataset, a collaborative effort between NOAA's Global Monitoring Laboratory (GML) and the Scripps Institution of Oceanography, is the designated final authority for prediction markets tracking atmospheric CO2 levels, particularly those forecasting concentrations before 2030 [^]. Many markets specifically reference daily average data from Mauna Loa [^]. NOAA GML provides comprehensive "Trends in CO2" data, offering daily, weekly, and monthly averages not only from Mauna Loa but also from other global sites [^]. The Mauna Loa CO2 flask data is especially important for defining the Keeling Curve and understanding the global carbon cycle [^].
NOAA's CO2 data undergoes explicit preliminary review and revision before finalization. NOAA GML explicitly states that its data are updated daily and remain "preliminary until reviewed," indicating that initial figures are subject to quality control and revision [^]. This process involves a thorough review of monthly mean CO2 concentrations from flask samples for quality assurance and the notation of any known issues [^]. Such ongoing quality control ensures that historical data points may be refined or adjusted due to factors like improved measurement techniques, updated calibration standards, or identified inconsistencies [^].
Market participants should expect minor adjustments to early reported numbers due to this rigorous process. While the overall trends in atmospheric CO2 concentration are expected to remain stable, market participants should be aware that early reported numbers, particularly those not yet finalized by NOAA GML, might undergo minor adjustments or recalibrations. These potential revisions could occur up to the resolution date in early 2030, as they are an integral part of rigorous scientific data management aimed at ensuring the highest accuracy of the long-term atmospheric CO2 record [^].

10. What Could Change the Odds

Key Catalysts

Catalyst analysis unavailable.

Key Dates & Catalysts

  • Expiration: January 16, 2030
  • Closes: January 01, 2030

11. Decision-Flipping Events

  • Trigger: Catalyst analysis unavailable.

13. Historical Resolutions

No historical resolution data available for this series.