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

Speciation Rates01:07

Speciation Rates

22.4K
Overview
22.4K
The Water Cycle01:00

The Water Cycle

27.9K
The Earth’s hydrosphere includes all of the areas where the storage and movement of water occurs. Since water is the basis of all living processes, the cycling of water is extremely important to ecosystem dynamics.
27.9K
Wave Parameters01:10

Wave Parameters

8.9K
The simplest mechanical waves are associated with simple harmonic motion and repeat themselves for several cycles. These simple harmonic waves can be modeled using a combination of sine and cosine functions. Consider a simplified surface water wave that moves across the water's surface. Unlike complex ocean waves, in surface water waves, water moves vertically, oscillating up and down, whereas the disturbance of the wave moves horizontally through the medium. If a seagull is floating on the...
8.9K
Mixing Time01:19

Mixing Time

360
The concept of mixing time is significant in producing a uniform concrete mix with the required strength. The mixing period starts once all components are in the mixer. Initially, the mixer is charged with 10% of the water, followed by the consistent addition of solids and then 80% of the water. The remaining water is added later, within the first quarter of the mixing period. The minimum mixing time varies according to the mixer's capacity; for example, mixers with up to 1 cubic yard...
360
What is an Ecosystem?01:17

What is an Ecosystem?

46.4K
Overview
46.4K
Gradually Varying Flow01:29

Gradually Varying Flow

313
Gradually varying flow (GVF) in open channels describes situations where water depth changes slowly along the channel due to factors like non-uniform bed slope, channel shape variations, or obstructions. This flow type occurs when the depth adjusts gradually to balance gravitational forces, shear forces, and energy requirements, resulting in a low rate of depth change.Characteristics of Gradually Varying FlowGVF is commonly observed in natural streams, rivers, and canals, where flow depth...
313

You might also read

Related Articles

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

Sort by
Same author

Seasonal productivity of the equatorial Atlantic shaped by distinct wind-driven processes.

Nature geoscience·2025
Same author

Prolonged thermocline warming by near-inertial internal waves in the wakes of tropical cyclones.

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

Physics-informed deep-learning parameterization of ocean vertical mixing improves climate simulations.

National science review·2022
Same author

Ocean feedback to pulses of the Madden-Julian Oscillation in the equatorial Indian Ocean.

Nature communications·2016
Same author

Corrigendum: The formation and fate of internal waves in the South China Sea.

Nature·2015
Same author

The formation and fate of internal waves in the South China Sea.

Nature·2015

Related Experiment Video

Updated: Dec 17, 2025

Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression
08:15

Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression

Published on: July 28, 2023

1.7K

Variations in Ocean Mixing from Seconds to Years.

James N Moum1

  • 1College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97330-5503, USA;

Annual Review of Marine Science
|July 1, 2020
PubMed
Summary

Ocean mixing is crucial for geophysical fluid dynamics. New measurement techniques reveal how turbulence, varying greatly in scale, drives mixing across diverse temporal scales from seconds to years.

Area of Science:

  • Geophysical Fluid Dynamics
  • Oceanography
  • Turbulence Research

Background:

  • Community-wide recognition of small-scale mixing's importance in geophysical fluid dynamics.
  • Significant scale separation between ocean basins and turbulent eddies.
  • Challenges in measuring and understanding ocean mixing due to sparse data.

Purpose of the Study:

  • To review recent and classic results on ocean mixing.
  • To explore the temporal variability of turbulence-enhanced mixing.
  • To connect turbulence timescales to larger oceanographic processes.

Main Methods:

  • Comprehensive shipboard turbulence profiling experiments.
  • Doppler sonar current measurements.
  • Analysis of data spanning minutes to years.
Keywords:
mixingtemporal variabilityturbulence

More Related Videos

Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

6.8K
The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
10:11

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations

Published on: August 3, 2016

10.3K

Related Experiment Videos

Last Updated: Dec 17, 2025

Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression
08:15

Author Spotlight: Unveiling Plankton Response to Climate Change Through Time-Series Data and Artistic Expression

Published on: July 28, 2023

1.7K
Evolution of Staircase Structures in Diffusive Convection
07:28

Evolution of Staircase Structures in Diffusive Convection

Published on: September 5, 2018

6.8K
The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations
10:11

The Benthic Exchange of O2, N2 and Dissolved Nutrients Using Small Core Incubations

Published on: August 3, 2016

10.3K

Main Results:

  • Detailed observations of upper-ocean turbulence vertical structure evolution.
  • Understanding of how turbulence varies across timescales (seconds to years).
  • Insights into mixing across tidal cycles, monsoons, seasons, and ENSO events.

Conclusions:

  • Temporal variability is key to understanding ocean mixing.
  • Advancements in measurement technology enable longer-term, detailed studies.
  • Expanded knowledge connects small-scale turbulence to large-scale ocean dynamics.