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| 001 | 521551 | ||
| 005 | 20240927184137.0 | ||
| 024 | 7 | _ | |a G:(GEPRIS)191683119 |d 191683119 |
| 035 | _ | _ | |a G:(GEPRIS)191683119 |
| 040 | _ | _ | |a GEPRIS |c http://gepris.its.kfa-juelich.de |
| 150 | _ | _ | |a Parameterisation of meso-scale mixing in the ocean |y 2011 - 2017 |
| 371 | _ | _ | |a Professor Dr. Carsten Eden |
| 450 | _ | _ | |a DFG project G:(GEPRIS)191683119 |w d |y 2011 - 2017 |
| 510 | 1 | _ | |a Deutsche Forschungsgemeinschaft |0 I:(DE-588b)2007744-0 |b DFG |
| 680 | _ | _ | |a Ocean models which do not resolve the energetic meso-scale eddy field have to parameterise its effects on the large-scale circulation. This effect is for instance important in western boundary currents, where meso-scale eddies balances the planetary vorticity change, and in the Southern Ocean where they control both the zonal ow and the meridional overturning circulation. Further, meso-scale eddies are important for the ventilation of the interior ocean with dissolved gases. In current ocean climate models, a constant lateral diffusivity K appropriate to the Gent and McWilliams (1990) parameterisation is used. However, a constant diffusivity K is inadequate for climate change simulations and decadal climate predictions, since K does vary both in time and in space. We propose to advance the current meso-scale eddy parameterisation in ocean climate models by applying and improving a mixing length approach for K, based on an eddy kinetic energy (EKE) budget, an eddy length scale and a vertical structure function. The parameters in the EKE budget and the structure function will be estimated using a global ocean model and its adjoint constraining the model and the closure to observational estimates. |
| 909 | C | O | |o oai:juser.fz-juelich.de:947282 |p authority:GRANT |p authority |
| 909 | C | O | |o oai:juser.fz-juelich.de:947282 |
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| 980 | _ | _ | |a AUTHORITY |
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