A decadal oscillation due to the coupling between an ocean circulation model and a thermodynamic sea-ice model
Clicks: 2
ID: 299658
1995
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Popular Article
0.3
/100
2 views
1 readers
AI Quality Assessment
Not analyzed
Readership in this journal
PopularRanked #337 of 1,397 articles by views in journal of marine research
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 1,397 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
A 3-dimensional, planetary-geostrophic, ocean general circulation model is coupled to a thermodynamic sea-ice model. The thermal coupling takes account of the insulating effect of the ice. A simple approach is taken in the case of the freshwater flux by allowing this to pass through the ice, except that some is used for snow accumulation. It is then modified by salinity rejection/dilution due to freezing/melting. The model has idealized box geometry extending 60° in both latitude and longitude, with a horizontal resolution of 2° and 14 vertical levels. Annual mean surface forcings are used. The coupled system is first spun up using restoring conditions on both surface temperature and surface salinity to reach a steady state which includes ice in the high latitudes. A switch of the surface forcing to mixed boundary conditions (restoring on temperature and flux on salinity) leads to an oscillation of period 17 years in the magnitude of the thermohaline circulation and the ice extent. The oscillation is due to a feedback between ice cover and ocean temperature. Since ice forms only in regions where the ocean loses heat to the atmosphere, the thermal insulation of an increased ice cover makes the ocean warmer. The thermohaline circulation plays a role in transporting this heat polewards, which in turn melts the ice. The heat loss over open water at high latitudes then leads to ice formation and the process repeats itself. Salinity rejection/dilution associated with ice formation/melting is shown to be of secondary importance in this oscillation. Rather, changes in surface salinity are dominated by changes in deep convection and the associated vertical mixing, which are themselves associated with the reduction in surface heat loss due to the insulating effect of the ice. As a consequence the model exhibits the negative correlation between surface salinity and ice extent that is observed in the high latitude North Atlantic
| Reference Key |
openalex_W2019943139
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Sheng Zhang, Charles A. Lin, Richard J. Greatbatch |
| Journal | journal of marine research |
| Year | 1995 |
| DOI |
10.1357/0022240953213304
|
| URL | |
| Keywords | Keywords not found |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.