by Daniel Brouse and Sidd Mukherjee
November 17, 2025
CO2 is only one component in a vast, interconnected climate system -- but it remains the most significant driver of human-caused warming. While water vapor, clouds, aerosols, and ocean circulation all play essential roles, CO2 is the primary forcing mechanism we directly control. And today, it is rising at a speed unprecedented in Earth's recent geological history.
According to the World Meteorological Organization (2025) and the Global Carbon Project (2025), the year 2024 marked the most extreme convergence of climate records ever observed. Atmospheric CO2 levels reached 422.7 ppm, the highest in three million years, with a record annual increase of 3.75 ppm. Monthly readings peaked at 426.91 ppm in June 2024 -- a value that would have been unimaginable even a generation ago.
Global fossil fuel and cement emissions rose to 37.4 gigatons of CO2 in 2024, a 0.8% increase from 2023. The growth was driven by:
Coal expansion across Asia
Post-pandemic industrial rebound
Sharp increases in liquefied natural gas (LNG) production, particularly in the United States
While often marketed as a "bridge fuel," methane leakage from LNG infrastructure -- over 80 times more potent than CO2 over 20 years -- has erased its supposed climate advantage. These cumulative emissions are now overwhelming the buffering capacity of the oceans, cryosphere, and biosphere.
This record convergence signals a fundamental phase transition in the Earth system. Regions that once absorbed carbon, stabilized temperature, and moderated climate extremes are now flipping into self-reinforcing feedback loops. What was once a slow climb in global heat content is now taking on the characteristics of nonlinear acceleration.
The WMO issued one of its starkest warnings in 2023:
"The world's glaciers melted at dramatic speed last year and saving them is effectively a lost cause…
Antarctic sea ice fell to its lowest extent on record.
Some European glaciers are literally off the charts."
WMO Secretary-General Petteri Taalas summarized the situation bluntly:
"We have already lost the melting-of-the-glaciers game.
The CO2 concentration is now simply too high."
In the Swiss Alps alone, 6.2% of total glacier mass vanished in a single summer, the greatest loss in the entire observational record.
Taalas further warned that disappearing glaciers will:
Reduce global freshwater supply
Impair agriculture
Destabilize river transport and hydrology
Accelerate sea-level rise far beyond prior projections
For decades, sea-level rise was expected to unfold over millennia. But with runaway CO2 growth and feedback amplification, that timeline is rapidly collapsing into decades.
A natural question follows:
Could this trigger the fastest sea-level rise in Earth's history?
Physicist Sidd Mukherjee offered the following expert assessment:
"It depends on what you mean by ‘ever.'
In terms of human civilization: yes, likely."
He notes:
The total global ice inventory can produce ~200 feet of sea-level rise.
Greenland and West Antarctica may already be committed to collapse.
Breakdown of likely contributions:
Greenland: ~20 feet over 100–300 years
West Antarctica: ~10 feet, potentially in decades to a century
Average over a century:
~20 feet → 2 inches per year (50 mm/year), 10x the current rate
But the average masks the danger. Sea-level rise will likely arrive in pulses, not a smooth curve:
"We could dawdle along at half an inch per year, then suddenly experience a couple of years with a foot of rise annually."
If CO2-equivalent concentrations can be stabilized near 500 ppm, there may still be a chance to preserve East Antarctica, the largest remaining ice sheet. But if it destabilizes:
"Expect another couple hundred feet of sea-level rise."
We are now witnessing the early stages of a global system crossing into a new and dangerous mode of operation -- one defined by:
Rapid CO2 accumulation
Collapsing carbon sinks
Accelerating ocean heat storage
Cryosphere destabilization
Intensified extreme weather
The question is no longer whether these changes are occurring, but how quickly, and how prepared we are for the consequences.
Humanity is approaching -- and in some cases passing -- thresholds that earlier generations believed were centuries away. The decisions made in the next decade will determine whether sea-level rise is measured in inches, feet, or tens of feet within a single human lifetime.
WARNING
* Our probabilistic, ensemble-based climate model -- which incorporates complex socio-economic and ecological feedback loops within a dynamic, nonlinear system -- projects that global temperatures are becoming unsustainable this century. This far exceeds earlier estimates of a 4°C rise over the next thousand years, highlighting a dramatic acceleration in global warming. We are now entering a phase of compound, cascading collapse, where climate, ecological, and societal systems destabilize through interlinked, self-reinforcing feedback loops.
What Can I Do?
The single most important action you can take to help address the climate crisis is simple: stop burning fossil fuels. There are numerous actions you can take to contribute to saving the planet. Each person bears the responsibility to minimize pollution, discontinue the use of fossil fuels, reduce consumption, and foster a culture of love and care. The Butterfly Effect illustrates that a small change in one area can lead to significant alterations in conditions anywhere on the globe. Hence, the frequently heard statement that a fluttering butterfly in China can cause a hurricane in the Atlantic. Be a butterfly and affect the world.