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

Radiation: Applications01:17

Radiation: Applications

1.3K
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.
The average...
1.3K
Radiation Pressure: Problem Solving01:09

Radiation Pressure: Problem Solving

465
The radiation pressure applied by an electromagnetic wave on a perfectly absorbing surface equals the energy density of the wave. The wave's momentum also gets transferred to the surface when an electromagnetic wave is entirely absorbed by it. The rate at which momentum is transmitted to an absorbing surface perpendicular to the propagation direction equals the force on the surface.
The average value of the rate of momentum transfer divided by the absorbing area represents the average force...
465
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

Influence of Earth's Curvature and Atmospheric Refraction on Leveling

293
During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance.
293
Absorption of Radiation01:05

Absorption of Radiation

832
The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
832
Global Climate Change01:50

Global Climate Change

24.8K
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.
24.8K
Apparent Weight and the Earth's Rotation01:28

Apparent Weight and the Earth's Rotation

3.7K
Since all objects on the Earth's surface move through a circle every 24 hours, there must be a net centripetal force on each object, directed towards the center of that circle. The points of the north and south poles are the only exception to this rule.
For an object on the Earth's equator, the net centripetal force that accounts for its rotation is the Earth's pull towards its center, or the weight minus the normal force that prevents it from piercing into the Earth's surface....
3.7K

You might also read

Related Articles

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

Sort by
Same author

Machine learning-based extreme event attribution.

Science advances·2024
Same author

Speed of environmental change frames relative ecological risk in climate change and climate intervention scenarios.

Nature communications·2024
Same author

Data-driven predictions of the time remaining until critical global warming thresholds are reached.

Proceedings of the National Academy of Sciences of the United States of America·2023
Same author

Internal variability and forcing influence model-satellite differences in the rate of tropical tropospheric warming.

Proceedings of the National Academy of Sciences of the United States of America·2022
Same author

Climate impact assessments should not discount 'hot' models.

Nature·2022
Same author

Past Variance and Future Projections of the Environmental Conditions Driving Western U.S. Summertime Wildfire Burn Area.

Earth's future·2021

Related Experiment Video

Updated: Sep 19, 2025

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

8.0K

Observation-based estimate of Earth's effective radiative forcing.

Senne Van Loon1, Maria Rugenstein1, Elizabeth A Barnes1

  • 1Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80521.

Proceedings of the National Academy of Sciences of the United States of America
|June 10, 2025
PubMed
Summary

Human emissions significantly impact Earth's climate. This study estimates effective radiative forcing using machine learning and observations, revealing a substantial increase since 2021, consistent with recent warming trends.

Keywords:
climateenergy budgetradiative forcing

More Related Videos

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

8.8K
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

8.1K

Related Experiment Videos

Last Updated: Sep 19, 2025

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites
09:05

Measurements of CO2 Fluxes at Non-Ideal Eddy Covariance Sites

Published on: June 24, 2019

8.0K
Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

8.8K
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

8.1K

Area of Science:

  • Climate Science
  • Earth System Science
  • Atmospheric Physics

Background:

  • Human emissions are a primary driver of climate change.
  • Effective radiative forcing (ERF) quantifies anthropogenic and natural impacts on Earth's energy balance.
  • Direct observation of ERF is challenging, necessitating reliance on climate models.

Purpose of the Study:

  • To develop an observational estimate of effective radiative forcing.
  • To utilize machine learning to bridge the gap between climate models and observational data.
  • To provide an independent assessment of ERF trends.

Main Methods:

  • Employed machine learning to model the relationship between surface temperature and radiation from internal climate variability.
  • Integrated multimodel ensemble data with observed surface temperature and net radiative imbalance.
  • Calculated the effective radiative forcing trend from 2001-2024.

Main Results:

  • Estimated an effective radiative forcing trend of 0.71 ± 0.21 Wm⁻² per decade for 2001-2024.
  • Demonstrated an independent assessment of observed ERF since 1985.
  • Showed a substantial increase in ERF since 2021, not offset by radiative response until 2024.

Conclusions:

  • The study provides a novel, observationally constrained estimate of effective radiative forcing.
  • Findings align with physical understanding of radiative feedbacks and recent exceptional warmth.
  • Advances the ability to close the Earth's energy budget on annual timescales.