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Related Concept Videos

What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
What is Weather?01:07

What is Weather?

Overview
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Clausius-Clapeyron Equation02:35

Clausius-Clapeyron Equation

The equilibrium between a liquid and its vapor depends on the temperature of the system; a rise in temperature causes a corresponding rise in the vapor pressure of its liquid. The Clausius-Clapeyron equation gives the quantitative relation between a substance’s vapor pressure (P) and its temperature (T); it predicts the rate at which vapor pressure increases per unit increase in temperature.

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Updated: Jul 3, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

A simple climate change model for the concerned public.

Philip J Wilson1

  • 1Independent researcher, Kent, UK.

UCL Open. Environment
|July 2, 2026
PubMed
Summary
This summary is machine-generated.

Simple trend line analysis of global warming data shows a consistent warming rate of approximately 0.20°C per decade. Extrapolating this trend suggests significant future temperature increases, aiding public understanding of climate change.

Keywords:
Intergovernmental Panel on Climate Changeconcerned publicglobal warmingpublic understanding of sciencescience educationsimplicity

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Last Updated: Jul 3, 2026

Using Generative Art to Convey Past and Future Climate Transitions
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Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

Area of Science:

  • Climate Science
  • Environmental Science
  • Data Analysis

Background:

  • Complex global warming models by the Intergovernmental Panel on Climate Change (IPCC) are often difficult for the public to grasp.
  • A simpler approach using trend lines in near-surface temperature data can provide accessible insights into global warming.

Purpose of the Study:

  • To analyze global mean annual near-surface warming using a simple linear trend line model.
  • To project future warming based on recent temperature data trends.
  • To bridge the gap between scientific reality and public perception of climate change.

Main Methods:

  • Analysis of global mean annual near-surface temperature data from 1974 to 2023.
  • Calculation of linear trend lines and mean rates of temperature increase per decade.
  • Extrapolation of the trend line to project future temperature increases.

Main Results:

  • The 50-year trend (1974-2023) shows a warming rate of 0.20°C per decade.
  • More recent 20-year and annual updates indicate slightly higher rates (0.21°C to 0.27°C per decade).
  • Linear projection of the 2005-2024 trend predicts +1.5°C by 2029 and +2°C by 2047.

Conclusions:

  • Simple linear trend analysis provides a practical and understandable index of global warming.
  • These accessible projections align with more complex climate models.
  • Demystifying climate data through simple methods can improve public understanding and engagement with climate change issues.