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Related Concept Videos

Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.
Threats to Biodiversity01:50

Threats to Biodiversity

There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
Conservation of Declining Populations02:07

Conservation of Declining Populations

Conservation of declining population focuses on ways of detecting, diagnosing, and halting a population decline. The approach uses methods to prevent populations from going extinct.
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.
Acceleration due to Gravity on Other Planets01:24

Acceleration due to Gravity on Other Planets

The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...

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Related Experiment Video

Updated: Jun 26, 2026

Prospecting Microbial Strains for Bioremediation and Probiotics Development for Metaorganism Research and Preservation
09:49

Prospecting Microbial Strains for Bioremediation and Probiotics Development for Metaorganism Research and Preservation

Published on: October 31, 2019

Prognosis for a sick planet.

Mark Maslin1

  • 1UCL Environment Institute, University College London. mmaslin@geog.ucl.ac.uk

Clinical Medicine (London, England)
|January 20, 2009
PubMed
Summary
This summary is machine-generated.

Global warming, driven by fossil fuel use, is a critical 21st-century issue causing rising temperatures and sea levels. Technological solutions exist to mitigate these severe impacts on human society and the planet.

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Last Updated: Jun 26, 2026

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Area of Science:

  • Climate Science
  • Environmental Science

Background:

  • The 21st century faces global warming as a paramount scientific challenge, impacting societal structures.
  • Human activities, particularly fossil fuel combustion since the Industrial Revolution, have demonstrably altered the global climate.
  • Past climate data indicates significant sensitivity of the current climate system to anthropogenic influences.

Purpose of the Study:

  • To highlight the critical nature of global warming as the most important science issue of the 21st century.
  • To underscore the sensitivity of the global climate system to human-induced changes.
  • To present the projected impacts of global warming on global temperatures and sea levels.

Main Methods:

  • Analysis of historical climate data to understand past climate changes.
  • Review of findings from the Intergovernmental Panel on Climate Change (IPCC) synthesis report (2007).
  • Assessment of the evidence for temperature and sea-level rise in the 20th century.

Main Results:

  • Global temperatures rose by 0.75°C and sea levels by 22 cm in the 20th century.
  • Projected 21st-century temperature increases range from 1.1°C to 6.4°C.
  • Sea levels may rise by 28-79 cm, with potential acceleration due to polar ice cap melt.
  • Increased frequency and intensity of extreme weather events like storms, floods, heat waves, and droughts are anticipated.

Conclusions:

  • Global warming presents devastating potential effects on human society.
  • The current climate system is highly sensitive to human-induced climate change.
  • Technological solutions are available to address the global warming crisis.