Jump to content
  • Member Statistics

    17,611
    Total Members
    7,904
    Most Online
    NH8550
    Newest Member
    NH8550
    Joined

Increasing ocean stratification over the past half-century


bdgwx
 Share

Recommended Posts

Yet another study with significant implications. 

Official: Li et al 2020: Increasing ocean stratification over the past half-century

Open access: use this link

News article: Mixing of the planet’s ocean waters is slowing down, speeding up global warming, study finds, Washington Post, September 29, 2020

Abstract: Seawater generally forms stratified layers with lighter waters near the surface and denser waters at greater depth. This stable configuration acts as a barrier to water mixing that impacts the efficiency of vertical exchanges of heat, carbon, oxygen and other constituents. Previous quantification of stratification change has been limited to simple differencing of surface and 200-m depth changes and has neglected the spatial complexity of ocean density change. Here, we quantify changes in ocean stratification down to depths of 2,000 m using the squared buoyancy frequency N2 and newly available ocean temperature/salinity observations. We find that stratification globally has increased by a substantial 5.3% [5.0%, 5.8%] in recent decades (1960–2018) (the confidence interval is 5–95%); a rate of 0.90% per decade. Most of the increase (~71%) occurred in the upper 200 m of the ocean and resulted largely (>90%) from temperature changes, although salinity changes play an important role locally.

This finding has a few implications.

  • Reduced heat transport into the ocean depths means more heat is available to drive atmospheric temperatures upward.
  • The faster warming of the ocean surface will reduce carbon uptake since uptake is inversely proportion to the ocean temperature thus resulting in less carbon buffering and an increase in the rate at which CO2 is accumulating in the atmosphere.
  • The rate at which additional energy is becoming available to tropical cyclones is increasing.
  • The increased stratification may disrupt the Atlantic Meridional Overturning Circulation causing it to slow down.

 

  • Like 2
Link to comment
Share on other sites

3 hours ago, bdgwx said:

Yet another study with significant implications. 

Official: Li et al 2020: Increasing ocean stratification over the past half-century

Open access: use this link

News article: Mixing of the planet’s ocean waters is slowing down, speeding up global warming, study finds, Washington Post, September 29, 2020

Abstract: Seawater generally forms stratified layers with lighter waters near the surface and denser waters at greater depth. This stable configuration acts as a barrier to water mixing that impacts the efficiency of vertical exchanges of heat, carbon, oxygen and other constituents. Previous quantification of stratification change has been limited to simple differencing of surface and 200-m depth changes and has neglected the spatial complexity of ocean density change. Here, we quantify changes in ocean stratification down to depths of 2,000 m using the squared buoyancy frequency N2 and newly available ocean temperature/salinity observations. We find that stratification globally has increased by a substantial 5.3% [5.0%, 5.8%] in recent decades (1960–2018) (the confidence interval is 5–95%); a rate of 0.90% per decade. Most of the increase (~71%) occurred in the upper 200 m of the ocean and resulted largely (>90%) from temperature changes, although salinity changes play an important role locally.

This finding has a few implications.

  • Reduced heat transport into the ocean depths means more heat is available to drive atmospheric temperatures upward.
  • The faster warming of the ocean surface will reduce carbon uptake since uptake is inversely proportion to the ocean temperature thus resulting in less carbon buffering and an increase in the rate at which CO2 is accumulating in the atmosphere.
  • The rate at which additional energy is becoming available to tropical cyclones is increasing.
  • The increased stratification may disrupt the Atlantic Meridional Overturning Circulation causing it to slow down.

 

This is a disturbing development. It will likely amplify the changes being driven by AGW. 

  • Like 1
Link to comment
Share on other sites

Create an account or sign in to comment

You need to be a member in order to leave a comment

Create an account

Sign up for a new account in our community. It's easy!

Register a new account

Sign in

Already have an account? Sign in here.

Sign In Now
 Share

  • Recently Browsing   0 members

    • No registered users viewing this page.
×
×
  • Create New...