Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

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.
Atomic Spectroscopy: Effects of Temperature01:27

Atomic Spectroscopy: Effects of Temperature

Atomization, converting samples into gas-phase atoms and ions, is essential for atomic spectroscopy. The flame temperature required for atomization affects the efficiency of the atomic spectroscopic methods by increasing the atomization efficiency and the relative population of the excited and ground states.
At thermal equilibrium, the relative populations of excited and ground state atoms can be estimated using the Maxwell–Boltzmann distribution. For example, an increase in temperature from...
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
Pressure and Volume in an Adiabatic Process01:27

Pressure and Volume in an Adiabatic Process

Free expansion of a gas is an adiabatic process. However, there are few differences between free expansion and adiabatic expansion. During free expansion, no work is done, and there is no change in internal energy. But, for an adiabatic expansion, work is done, and there is a change in internal energy. During an adiabatic process, the relation between the pressure and volume is obtained from the condition for the adiabatic process, that is,

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Solubilities of dodecyl- and octadecyl-trimethyl-ammonium chlorides in organic solvents.

The Journal of organic chemistry·2010
Same author

The preparation and properties of several isomeric unsymmetrical anhydrides of the saturated aliphatic monocarboxylic acids.

The Journal of organic chemistry·2010
Same author

Stratospheric ozone effects on temperature.

Science (New York, N.Y.)·1976
Same author

Influence of aerosol cloud height on the change in the atmospheric radiation balance due to aerosols.

Atmospheric environment·1975
Same author

Aerosols in the atmosphere: calculation of the critical absorption/backscatter ratio.

Science (New York, N.Y.)·1974

Related Experiment Video

Updated: Jul 12, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
06:27

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

Published on: May 29, 2019

Aerosols and polar temperature changes.

R A Reck

    Science (New York, N.Y.)
    |May 16, 1975
    PubMed
    Summary

    Aerosols do not explain the current rise in Northern Hemisphere ice. Instead, these atmospheric particles appear to warm polar regions, with greater warming observed at the South Pole.

    Area of Science:

    • Atmospheric science
    • Climate science
    • Polar research

    Background:

    • Understanding the drivers of polar ice changes is crucial for climate modeling.
    • The role of atmospheric aerosols in polar climate dynamics requires further investigation.

    Purpose of the Study:

    • To determine if aerosols are the cause of increased Northern Hemisphere ice.
    • To investigate the atmospheric temperature effects of aerosols in polar regions.

    Main Methods:

    • Utilized computational calculations to model aerosol impacts.
    • Analyzed aerosol density at high latitudes (85°S and 85°N).

    Main Results:

    • Calculations show aerosols are not directly responsible for increased Northern Hemisphere ice.

    More Related Videos

    Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions
    05:45

    Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

    Published on: January 7, 2019

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
    10:22

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

    Published on: September 7, 2019

    Related Experiment Videos

    Last Updated: Jul 12, 2026

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
    06:27

    Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer

    Published on: May 29, 2019

    Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions
    05:45

    Composition and Distribution Analysis of Bioaerosols Under Different Environmental Conditions

    Published on: January 7, 2019

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
    10:22

    Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

    Published on: September 7, 2019

  • Aerosols were found to cause atmospheric heating near the poles.
  • A 0.2 K temperature increase was observed at 85°S due to background aerosol density.
  • A 0.05 K temperature increase was observed at 85°N due to background aerosol density.
  • Conclusions:

    • Aerosols do not directly cause the observed increase in Northern Hemisphere ice.
    • Aerosols contribute to polar atmospheric warming, with a more significant effect in the Southern Hemisphere polar region.