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Related Concept Videos

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.
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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...
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Applications of GIS: Disaster Management and Emergency Response01:29

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Geographic Information System (GIS) technology is essential for risk identification, action prioritization, and resource optimization in critical situations like flooding and earthquakes. By integrating spatial and demographic data, GIS provides a comprehensive framework for emergency response.GIS integrates data layers, like rainfall intensity, topography, elevation profiles, and river levels, to model high-risk flood zones. These layers assess areas susceptible to flooding based on their...
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Radiation: Applications01:17

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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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Using Generative Art to Convey Past and Future Climate Transitions
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Potential for a hazardous geospheric response to projected future climate changes.

B McGuire1

  • 1Aon Benfield UCL Hazard Research Centre, Department of Earth Sciences, University College London, Gower Street, London WC1E 6BT, UK. w.mcguire@ucl.ac.uk

Philosophical Transactions. Series A, Mathematical, Physical, and Engineering Sciences
|April 21, 2010
PubMed
Summary

Global warming is increasing geological and geomorphological hazards. Research is needed to understand climate change impacts on Earth

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Area of Science:

  • Earth Science
  • Climate Science
  • Geology

Background:

  • Exceptional climate change events in Earth's history correlate with heightened geological and geomorphological activity.
  • This activity includes volcanic eruptions, seismic events, landslides, tsunamis, floods, debris flows, and gas-hydrate destabilization.

Purpose of the Study:

  • To review the potential influences of anthropogenic warming on geological and geomorphological hazards.
  • To advocate for focused research to better understand these mechanisms, identify susceptible regions, and assess societal impacts.

Main Methods:

  • Review of existing literature and modeling studies on climate change and geological hazards.
  • Analysis of current trends and observational data linking global temperature rise to geospheric responses.

Main Results:

  • Modeling studies and trend projections indicate an increased risk of geological and geomorphological hazards in a warming world.
  • Observations suggest that rising global temperatures may already be triggering hazardous geospheric responses.

Conclusions:

  • Anthropogenic climate change poses a growing risk of geological and geomorphological hazards.
  • Further research is crucial to understand the mechanisms, susceptibility, and impacts of these hazards for society and infrastructure.