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Related Concept Videos

Newtonian Fluid: Problem Solving01:18

Newtonian Fluid: Problem Solving

Newtonian fluids exhibit a constant viscosity, meaning their shear stress and shear strain rate are directly proportional. This property ensures a predictable and stable response to applied forces, maintaining a linear relationship between force and flow. Examples include water, air, and light oils, consistently demonstrating this proportional behavior regardless of external conditions.
A velocity gradient forms within the fluid when a Newtonian fluid is placed between two parallel plates, with...
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...
Isochoric and Isobaric Processes01:21

Isochoric and Isobaric Processes

A thermodynamic process that occurs at constant volume is called an isochoric process. According to the first law of thermodynamics, heat supplied or removed from the system is partially utilized to perform work and change the internal energy of the system. However, in an isochoric process, the volume remains constant. Hence, the work done by the system is zero. Therefore, the exchange of heat changes the internal energy of the system only. 
Suppose 1000 g of water is heated from 40 degrees...
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.
Magnetostatic Boundary Conditions01:28

Magnetostatic Boundary Conditions

An electric field suffers a discontinuity at a surface charge. Similarly, a magnetic field is discontinuous at a surface current. The perpendicular component of a magnetic field is continuous across the interface of two magnetic mediums. In contrast, its parallel component, perpendicular to the current, is discontinuous by the amount equal to the product of the vacuum permeability and the surface current. Like the scalar potential in electrostatics, the vector potential is also continuous...
Turbulent Flow: Problem Solving01:09

Turbulent Flow: Problem Solving

Carbonation is a process used to dissolve carbon dioxide gas in a liquid, commonly used in the production of carbonated beverages. Achieving efficient carbonation requires careful control of temperature, pressure, and flow conditions. By adjusting these parameters, carbonation efficiency can be maximized, producing a higher concentration of CO2 in the liquid.
Temperature is a key factor in CO2 solubility. In this case, the CO2 gas and the liquid are cooled to 20°C. Lower temperatures enhance...

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Related Experiment Video

Updated: Jun 14, 2026

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

Data-driven global ocean model resolving atmospherically forced ocean dynamics.

Jeong-Hwan Kim1, Daehyun Kang1, Young-Min Yang2

  • 1Center for Climate and Carbon Cycle Research, Korea Institute of Science and Technology, Seoul, Republic of Korea.

Science Advances
|June 12, 2026
PubMed
Summary
This summary is machine-generated.

Deep learning models show promise for long-range climate prediction by accurately simulating ocean dynamics. KIST-Ocean, a new deep learning ocean model, captures key atmospheric-ocean interactions for improved forecasting.

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Using Generative Art to Convey Past and Future Climate Transitions

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Related Experiment Videos

Last Updated: Jun 14, 2026

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

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
10:28

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information

Published on: June 13, 2020

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

Area of Science:

  • Earth System Science
  • Climate Modeling
  • Artificial Intelligence in Geosciences

Background:

  • Traditional numerical weather models struggle with subseasonal to seasonal (S2S) climate predictions.
  • Accurate simulation of ocean-atmosphere interactions is crucial for extending forecast timescales.
  • Deep learning (DL) offers potential for more efficient and accurate climate modeling.

Purpose of the Study:

  • To introduce KIST-Ocean, a novel deep learning-based global ocean general circulation model.
  • To evaluate the simulation skill and efficiency of KIST-Ocean.
  • To demonstrate the model's capability in reproducing key ocean-atmosphere dynamics relevant to climate phenomena.

Main Methods:

  • Development of a deep learning-based global three-dimensional ocean general circulation model (KIST-Ocean).
  • Comprehensive evaluation of KIST-Ocean's performance against established benchmarks.
  • Analysis of the model's ability to simulate specific ocean responses like wave propagation and vertical motions.

Main Results:

  • KIST-Ocean demonstrates robust ocean simulation skill and high computational efficiency.
  • The model accurately reproduces atmospherically forced ocean dynamics, including Kelvin and Rossby waves.
  • KIST-Ocean successfully simulates vertical motions driven by wind stress curl, crucial for phenomena like ENSO.

Conclusions:

  • Deep learning models, like KIST-Ocean, can effectively capture essential ocean-atmosphere relationships.
  • These findings enhance confidence in DL-based global weather and climate models.
  • KIST-Ocean provides a foundation for developing integrated Earth system models for advanced long-range climate prediction.