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

24.0K
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.
24.0K
What is Climate?01:16

What is Climate?

18.1K
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.
18.1K
Radiation: Applications01:17

Radiation: Applications

1.1K
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...
1.1K
Mechanisms of Heat Transfer II01:20

Mechanisms of Heat Transfer II

3.1K
In convection, thermal energy is carried by the large-scale flow of matter. Ocean currents and large-scale atmospheric circulation, which result from the buoyancy of warm air and water, transfer hot air from the tropics toward the poles and cold air from the poles toward the tropics. The Earth’s rotation interacts with those flows, causing the observed eastward flow of air in the temperate zones. Convection dominates heat transfer by air, and the amount of available space for the airflow...
3.1K
Conduction, Convection and Radiation: Problem Solving01:20

Conduction, Convection and Radiation: Problem Solving

1.1K
There are three methods by which heat transfer can take place: conduction, convection, and radiation. Each method has unique and interesting characteristics, but all three have two things in common: they transfer heat solely because of a temperature difference; and the greater the temperature difference, the faster the heat transfer.
In order to solve a problem related to heat transfer, first of all, the situation needs to be examined to determine the type of heat transfer involved. This could...
1.1K
What is Weather?01:07

What is Weather?

17.9K
Overview
17.9K

You might also read

Related Articles

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

Sort by
Same author

Transfer learning reveals large discrepancies between air and land surface temperatures in cities.

Nature communications·2026
Same author

Differentiable land model reveals global environmental controls on latent ecological functions.

Nature communications·2026
Same author

Leaf temperature and its departure from ambient air temperature.

Nature plants·2026
Same author

Thermodynamically consistent machine learning model for excess Gibbs energy.

Nature communications·2026
Same author

Physically consistent global atmospheric data assimilation with machine learning in latent space.

Science advances·2026
Same author

A near-real time daily European Power Consumption and Carbon Intensity Dataset (ECON-PowerCI).

Scientific data·2025
Same journal

Tau protein as a regulator of mitochondrial function and dynamics.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same journal

A scalable, dividing cell model for the robust propagation and quantification of human sporadic Creutzfeldt-Jakob disease prions.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same journal

Epigenetic regulation of mesenchymal BMP signaling directs postnatal organ innervation.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same journal

Single-shot wide-field biochemical imaging at 1 kHz frame rate.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same journal

Morphogenesis and topological evolution of a frustrated nematic liquid crystal under confinement.

Proceedings of the National Academy of Sciences of the United States of America·2026
Same journal

B cell-intrinsic CXCR3 drives efficient generation of ectopic pulmonary germinal center responses to influenza A virus infection.

Proceedings of the National Academy of Sciences of the United States of America·2026
See all related articles

Related Experiment Video

Updated: May 15, 2025

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

828

Transferring climate change physical knowledge.

Francesco Immorlano1,2,3, Veronika Eyring4,5, Thomas le Monnier de Gouville6,7

  • 1Centro Euro-Mediterraneo sui Cambiamenti Climatici Foundation - Euro-Mediterranean Center on Climate Change, Lecce 73100, Italy.

Proceedings of the National Academy of Sciences of the United States of America
|April 8, 2025
PubMed
Summary
This summary is machine-generated.

Machine learning, using a Transfer Learning approach, significantly reduces uncertainty in 21st-century global surface air temperature projections by merging Earth system model data with historical observations. This method improves regional patterns and narrows projections, aiding climate adaptation efforts.

Keywords:
CMIP6Machine Learningprojectionstemperatureuncertainty

More Related Videos

Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

2.8K
Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

8.7K

Related Experiment Videos

Last Updated: May 15, 2025

Using Generative Art to Convey Past and Future Climate Transitions
06:10

Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

828
Simulating Temperature in a Soil Incubation Experiment
08:39

Simulating Temperature in a Soil Incubation Experiment

Published on: October 28, 2022

2.8K
Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

8.7K

Area of Science:

  • Climate Science
  • Machine Learning Applications
  • Earth System Modeling

Background:

  • Reliable climate projections are crucial for adaptation and mitigation strategies.
  • Current Earth system models possess significant uncertainties, limiting projection accuracy.
  • Existing methods struggle to capture the climate system's nonlinear complexity.

Purpose of the Study:

  • To reduce the uncertainty spread in 21st-century global surface air temperature projections.
  • To leverage Machine Learning for optimal merging of Earth system model simulations and historical observations.
  • To improve regional temperature pattern accuracy in climate projections.

Main Methods:

  • Utilized a Transfer Learning approach within Machine Learning.
  • Integrated knowledge from global temperature maps simulated by Earth system models.
  • Incorporated observed historical temperature data to train the model.

Main Results:

  • Achieved an uncertainty reduction of over 50% compared to state-of-the-art methods.
  • Demonstrated improved regional temperature patterns in projections.
  • Provided narrower projections uncertainty crucial for climate adaptation.

Conclusions:

  • Machine Learning, specifically Transfer Learning, offers a powerful tool to enhance climate projection reliability.
  • The developed method effectively reduces uncertainty and improves regional detail in temperature projections.
  • This approach is vital for informing effective climate adaptation and mitigation planning.