Anthropogenic Global Warming: Evidence and Mechanisms of Human-Induced Climate Change

Daniel Brouse and Sidd Mukherjee
February 14, 2026

Human-induced climate change, also called anthropogenic global warming, is a physical phenomenon rooted in the radiative properties of greenhouse gases (GHGs), especially CO₂, CH₄, and N₂O, and their interaction with Earth’s energy balance.

1. The Greenhouse Effect

Earth receives energy from the Sun primarily in the form of shortwave radiation (visible light and near-infrared). The planet absorbs this energy and re-emits it as longwave infrared radiation. Greenhouse gases in the atmosphere absorb some of this infrared radiation and re-emit it, warming the lower atmosphere and surface. This is the greenhouse effect, and it is governed by fundamental physics:

Net Radiation=4S(1α)σT4

Where:

Without GHGs, Earth’s surface would average ~255 K (-18°C). With current GHG levels, it averages ~288 K (~15°C).

2. Human Contribution via CO₂

Humans have increased atmospheric CO₂ from ~280 ppm (pre-industrial) to ~420 ppm today. This increase is not from natural sources but primarily from burning fossil fuels (coal, oil, gas) and land-use changes. The isotopic signature of carbon identifies the source:

3. Radiative Forcing

Radiative forcing (ΔF\Delta F) quantifies how much a GHG changes the balance between incoming and outgoing radiation:

Explanation:

Where:

This formula captures the logarithmic relationship: each doubling of CO₂ produces roughly the same increase in radiative forcing (~3.7 W/m² per doubling).

Other gases:

The total forcing is the sum of all anthropogenic contributions:

Explanation:

4. Feedbacks Amplifying Warming

Initial radiative forcing is amplified by feedbacks:

This creates nonlinear acceleration: warming triggers processes that produce more warming — a key insight in the “Domino Effect” hypothesis.

5. Observational Evidence

  1. Rising global temperatures (surface and ocean heat content)

  2. Melting glaciers and ice sheets (Greenland, Antarctica, Arctic sea ice)

  3. Rising sea levels

  4. Atmospheric CO₂ increase with fossil fuel isotopic signature

  5. Measured radiative forcing matches predictions from CO₂ and other GHGs

Summary

Tipping points and feedback loops drive the acceleration of climate change. When one tipping point is toppled and triggers others, the cascading collapse is known as the Domino Effect.