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Take-a-Picture-Best-Of.mp3
[Intro]
[Refrain]
[Bridge]
[Refrain]
[Bridge]
[Refrain]
[Outro]
ABOUT THE SONG AND SCIENCE
Our ensemble-based probabilistic climate model integrates socio-economic, ecological, and biogeophysical feedbacks within a nonlinear dynamical system. The results indicate that global temperatures are on course to become unsustainable within this century, far surpassing earlier projections of a 4°C rise over a millennium26*.
The transition from a stable Holocene equilibrium to a runaway Anthropocene trajectory is characterized by compounding, interdependent feedbacks across multiple systems — thermal, hydrological, biological, and societal.
The events of 2024–2025 reveal the limits of incremental mitigation. Stabilizing Earth’s climate now demands more than emission reductions — it requires active carbon removal, ecosystem restoration, and an immediate global phase-out of fossil fuels.
As the planet’s natural stabilizers fail, humanity faces a critical juncture: continue deferring action or act decisively to preserve habitability. The evidence is unequivocal — the feedback loops have tipped, the tipping points have cascaded, and the window for prevention is rapidly closing.
26* 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.
From the album “Taken“
By Take-a-Picture-Best-Of.mp3
[Intro]
[Refrain]
[Bridge]
[Refrain]
[Bridge]
[Refrain]
[Outro]
ABOUT THE SONG AND SCIENCE
Our ensemble-based probabilistic climate model integrates socio-economic, ecological, and biogeophysical feedbacks within a nonlinear dynamical system. The results indicate that global temperatures are on course to become unsustainable within this century, far surpassing earlier projections of a 4°C rise over a millennium26*.
The transition from a stable Holocene equilibrium to a runaway Anthropocene trajectory is characterized by compounding, interdependent feedbacks across multiple systems — thermal, hydrological, biological, and societal.
The events of 2024–2025 reveal the limits of incremental mitigation. Stabilizing Earth’s climate now demands more than emission reductions — it requires active carbon removal, ecosystem restoration, and an immediate global phase-out of fossil fuels.
As the planet’s natural stabilizers fail, humanity faces a critical juncture: continue deferring action or act decisively to preserve habitability. The evidence is unequivocal — the feedback loops have tipped, the tipping points have cascaded, and the window for prevention is rapidly closing.
26* 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.
From the album “Taken“