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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.
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.
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Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
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...
Requirements for Human Life01:26

Requirements for Human Life

The Earth and its atmosphere have provided humans with air, water, and food, but these are not the only requirements for survival. Humans also require a specific range of temperature and pressure that the Earth and its atmosphere provides.
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Related Experiment Video

Updated: May 17, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
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Long-term variations in the surface air 7Be concentration and climatic changes.

Liu Jiwen1, Valeriia N Starovoitova, Douglas P Wells

  • 1Idaho State University, Idaho Accelerator Center, 1500 Alvin Ricken Dr., Pocatello, ID 83201, USA.

Journal of Environmental Radioactivity
|October 30, 2012
PubMed
Summary

Global beryllium-7 (7Be) surface concentrations show a decreasing trend over 25 years, possibly linked to atmospheric transport changes. A weak negative correlation with precipitation was also noted.

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Area of Science:

  • Environmental Science
  • Atmospheric Chemistry
  • Geochemistry

Background:

  • Beryllium-7 (7Be) is a cosmogenic radionuclide with a known atmospheric source.
  • Surface Air Sampling Program (SASP) data provides long-term measurements of atmospheric radionuclides.
  • Understanding 7Be trends can offer insights into atmospheric transport processes.

Purpose of the Study:

  • To analyze the long-term trend of 7Be surface concentration.
  • To investigate correlations between 7Be trends and climatic changes, specifically precipitation and temperature.
  • To assess the influence of atmospheric transport on 7Be distribution.

Main Methods:

  • Utilized EML Surface Air Sampling Program (SASP) data from 23 global sites.
  • Analyzed 7Be concentration data spanning over 25 years.
  • Employed two independent techniques to extract long-term trend parameters.

Main Results:

  • A pronounced decreasing trend in 7Be concentrations was observed at most stations.
  • A weak negative correlation between 7Be concentration and precipitation amount was identified.
  • Potential statistically significant changes in the atmospheric transport of 7Be were indicated.

Conclusions:

  • The observed decreasing trend in 7Be suggests alterations in atmospheric transport mechanisms.
  • Climate variables, particularly precipitation patterns, may weakly influence 7Be surface concentrations.
  • Further data from more globally representative sites are required to confirm the statistical robustness of these findings.