دورية أكاديمية

Assessment of the Finite-VolumE Sea ice–Ocean Model (FESOM2.0) – Part 2: Partial bottom cells, embedded sea ice and vertical mixing library CVMix

التفاصيل البيبلوغرافية
العنوان: Assessment of the Finite-VolumE Sea ice–Ocean Model (FESOM2.0) – Part 2: Partial bottom cells, embedded sea ice and vertical mixing library CVMix
المؤلفون: P. Scholz, D. Sidorenko, S. Danilov, Q. Wang, N. Koldunov, D. Sein, T. Jung
المصدر: Geoscientific Model Development, Vol 15, Pp 335-363 (2022)
بيانات النشر: Copernicus Publications, 2022.
سنة النشر: 2022
المجموعة: LCC:Geology
مصطلحات موضوعية: Geology, QE1-996.5
الوصف: The second part of the assessment and evaluation of the unstructured-mesh Finite-volumE Sea ice–Ocean Model version 2.0 (FESOM2.0) is presented. It focuses on the performance of partial cells and embedded sea ice and the effect of mixing parameterisations available through the Community Vertical Mixing (CVMix) package. It is shown that partial cells and embedded sea ice lead to significant improvements in the representation of the Gulf Stream and North Atlantic Current and the circulation of the Arctic Ocean. In addition to the already existing Pacanowski and Phillander (fesom_PP) and K-profile (fesom_KPP) parameterisations for vertical mixing in FESOM2.0, we document the impact of several mixing parameterisations from the CVMix project library. Among them are the CVMix versions of Pacanowski and Phillander (cvmix_PP) and K-profile (cvmix_KPP) parameterisations; the tidal mixing parameterisation (cvmix_TIDAL); a vertical mixing parameterisation based on turbulent kinetic energy (cvmix_TKE); and a combination of cvmix_TKE and the recent scheme for the computation of the Internal Wave Dissipation, Energy, and Mixing (IDEMIX) parameterisation. IDEMIX parameterises the redistribution of internal wave energy through wave propagation, non-linear interactions and the associated imprint on the vertical background diffusivity. Further, the benefit from using a parameterisation of Southern Hemisphere sea ice melt season mixing in the surface layer (MOMIX) for reducing Southern Ocean hydrographic biases in FESOM2.0 is presented. We document the implementation of different model components and illustrate their behaviour. This paper serves primarily as a reference for FESOM users but is also useful to the broader modelling community.
نوع الوثيقة: article
وصف الملف: electronic resource
اللغة: English
تدمد: 1991-959X
1991-9603
Relation: https://gmd.copernicus.org/articles/15/335/2022/gmd-15-335-2022.pdf; https://doaj.org/toc/1991-959X; https://doaj.org/toc/1991-9603
DOI: 10.5194/gmd-15-335-2022
URL الوصول: https://doaj.org/article/4693beb70c9f441bbf8407b2529749f6
رقم الأكسشن: edsdoj.4693beb70c9f441bbf8407b2529749f6
قاعدة البيانات: Directory of Open Access Journals
الوصف
تدمد:1991959X
19919603
DOI:10.5194/gmd-15-335-2022