The Geological Society of London—the UK’s professional association for geologists, founded in 1807—puts the rate of modern climate change into geological perspective:
“...the current speed of human-induced CO₂ change and warming is nearly without precedent in the entire geological record, with the only known exception being the instantaneous, meteorite-induced event that caused the extinction of non-bird-like dinosaurs 66 million years ago.”
Feedback loops amplify climate change and can push interconnected Earth systems past critical tipping points. As tipping points are crossed, they can trigger additional feedback loops and destabilize other climate systems. This cascading "Domino Effect" compresses timescales, accelerates change, and increases the risk of rapid, nonlinear climate transformations.
Backyard Experiments How Is the Climate Energy Hitting You? is a collection of backyard experiments conducted in conjunction with you—the reader. The goal is simple: to look at how the increased energy in the climate system is showing up in our everyday lives.
Is it becoming more extreme, more frequent, and more persistent? Are the changes becoming stranger—or even disturbing?
Climate Change Today: When Weather Becomes Climate is a three-part series designed to simplify where climate science stands today.
Much of the public discussion still focuses on historical trends and older climate models. But since 2023–2024, our understanding of the climate system has advanced significantly as scientists have increasingly examined real-time observations, accelerating changes, feedback loops, and complex Earth system behavior.
The goal of this series is to explain why understanding climate acceleration no longer requires multiple advanced degrees or a deep background in nonlinear chaos theory. The evidence is increasingly visible in the world around us. In many ways, you can begin by simply looking out your window.
🌎 Today — System-Wide Coupling: Analyzing how multiple climate feedbacks interact, reinforce one another, and amplify changes throughout the Earth system.
The implications are significant: examining individual climate indicators is no longer enough. We must increasingly measure how the entire climate system is changing, how its feedbacks are interacting, and how rapidly those interactions are evolving.
We are moving from measuring climate change to measuring the changing dynamics of climate change itself.
The question is no longer just how much the planet is warming.
It's how fast the processes driving that warming are changing.
The most significant emerging climate feedback accelerating the planetary energy imbalance is the decline in low-level clouds. Low-Level Cloud Overview
The only effective way to stop the acceleration of climate change is through the reduction of fossil-fuel combustion.
However, the most likely way of reversing the trajectory of climate change is through people using AI to develop previously unthought-of methods and technologies that can fundamentally change how we produce, consume, and manage resources—and potentially remove greenhouse gases from the atmosphere.
We examine how human activities — such as deforestation, fossil fuel combustion, mass consumption, industrial agriculture, and land development — interact with ecological processes like thermal energy redistribution, carbon cycling, hydrological flow, biodiversity loss, and the spread of disease vectors. These interactions do not follow linear cause-and-effect patterns. Instead, they form complex, self-reinforcing feedback loops that can trigger rapid, system-wide transformations — often abruptly and without warning. Grasping these dynamics is crucial for accurately assessing global risks and developing effective strategies for long-term survival.
