Over het archief
Het OWA, het open archief van het Waterbouwkundig Laboratorium heeft tot doel alle vrij toegankelijke onderzoeksresultaten van dit instituut in digitale vorm aan te bieden. Op die manier wil het de zichtbaarheid, verspreiding en gebruik van deze onderzoeksresultaten, alsook de wetenschappelijke communicatie maximaal bevorderen.
Dit archief wordt uitgebouwd en beheerd volgens de principes van de Open Access Movement, en het daaruit ontstane Open Archives Initiative.
Basisinformatie over ‘Open Access to scholarly information'.
one publication added to basket [329306] |
Full‐depth global estimates of ocean mesoscale eddy mixing from observations and theory
Groeskamp, S.; LaCasce, J.H.; McDougall, T.J.; Rogé, M. (2020). Full‐depth global estimates of ocean mesoscale eddy mixing from observations and theory. Geophys. Res. Lett. 47(18): e2020GL089425. https://dx.doi.org/10.1029/2020GL089425
In: Geophysical Research Letters. American Geophysical Union: Washington. ISSN 0094-8276; e-ISSN 1944-8007, meer
| |
Author keywords |
Mesoscale; Eddies Mixing; Paramterization; Tracer Transport; Eddy Kinetic Energy; Climate |
Auteurs | | Top |
- Groeskamp, S., meer
- LaCasce, J.H.
- McDougall, T.J.
- Rogé, M.
|
|
|
Abstract |
Mixing by mesoscale eddies profoundly impacts climate and ecosystems by redistributing and storing dissolved tracers such as heat and carbon. Eddy mixing is parameterized in most numerical models of the ocean and climate. To reduce known sensitivity to such parameterizations, observational estimates of mixing are needed. However, logistical and technological limitations obstruct our ability to measure global time‐varying mixing rates. Here, we extend mixing length theory with mean‐flow suppression theory, and first surface modes, to estimate mixing from readily‐available observational‐based climatological data, of salinity, temperature, pressure and eddy kinetic energy at the sea surface. The resulting full‐depth global maps of eddy mixing can reproduce the few available direct estimates and confirm the importance of mean‐flow suppression of mixing. The results also emphasize the significant effect of eddy surface intensification and its relation to the vertical density stratification. These new insights in mixing dynamics will improve future mesoscale eddy mixing parameterizations. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.