[PDF] Top 20 Entrenamiento de las pruebas de velocidad en natación
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The Finite-volumE Sea ice–Ocean Model (FESOM2)
... of finite-volume discretization are used at present in global ocean circulation ...unstructured-mesh finite-volume dis- cretization will reveal the most efficient ...ture model ... See full document
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Assessment of the Finite-volumE Sea ice-Ocean Model (FESOM2.0) – Part 1: Description of selected key model elements and comparison to its predecessor version
... and model element description of the second version of the unstructured-mesh Finite-volumE Sea ice-Ocean Model ...the model takes advantage of the ... See full document
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Scalability and some optimization of the Finite-volumE Sea ice–Ocean Model, Version 2.0 (FESOM2)
... ◦ ocean mesh with about 1 million wet surface vertices starts to saturate beyond 500 cores ...Parallel Ocean Program (POP) model starts to saturate after 4000 cores at ...unstructured-mesh ... See full document
8
Results from the implementation of the Elastic Viscous Plastic sea ice rheology in HadCM3
... In ocean-ice models forced by observed atmospheric fields, it is common to tune P* by comparing against buoy data (or against observed ice thickness and other parame- ters (Miller at ...coupled ... See full document
12
Sea ice thermohaline dynamics and biogeochemistry in the Arctic Ocean: empirical and model results
... in sea ice samples collected in the types of ice and periods simulated in this study [Olsen et ...the sea ice model is forced by atmospheric and oceanographic time series that in ... See full document
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The middle atmospheric circulation of a tidally locked Earth-like planet and the role of the sea surface temperature
... Gravity waves are also generated through interaction between the planet’s surface orography and the lower tropospheric wind field (Nappo 2013). The encounter between the tropospheric wind and a hill, mountain or mountain ... See full document
9
Highly branched isoprenoids for Southern Ocean sea ice reconstructions: a pilot study from the Western Antarctic Peninsula
... in sea ice at the WAP (King, 2014; King and Harangozo, 1998), we suggest that the biomarker data of the surface sediments relate to spring sea ice cover, which must have been enhanced compared ... See full document
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Atlantic waters inflow north of Svalbard: insights from IAOOS observations and Mercator Ocean global operational system during N ICE2015
... Mercator Ocean for the Coperni- cus Marine Environment Monitoring Service (CMEMS; ...the Ocean) [Madec, 2008] platform and uses a mul- tidata and multivariate reduced order Kalman filter based on the ... See full document
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CSIB v1 (Canadian Sea-ice Biogeochemistry): a sea-ice biogeochemical model for the NEMO community ocean modelling framework
... ecosystem model and as- sociated sea-ice biogeochemistry and pelagic sulfur-cycle ...indicate ice–ocean fluxes of nitrate (NO 3 ), ammonium (NH 4 ), ice algae (IA) and large ... See full document
26
Finite-Element Sea Ice Model (FESIM), version 2
... between ice volumes very much, but have substantial impact on the field of ...stronger ice (smaller 1) in the northwest corner, which is partly made weaker by increased number of Picard ... See full document
7
Arctic amplification under global warming of 1.5 and 2 °C in NorESM1-Happi
... smaller sea-ice extent and conversely underestimate the largest extent in the PD cli- ...having ice-free conditions when going from ...coupled model is too cold. It produces too much ... See full document
7
Block Approach to the Simulation of Circulation and Tides in the Black Sea
... the ocean thermohydrodynamics equations are written in a special symmetrized ...tasks. Finite-difference approximations of the equations are based on the C ... See full document
68
Description of the Earth system model of intermediate complexity LOVECLIM version 1.2
... Fig. 5. Schematic representation of the main processes described in the LOCH model (Mouchet, 2010). The left panel focuses on purely biological processes, while the right panel shows the processes affecting the ... See full document
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The Canadian Earth System Model version 5 (CanESM5.0.3)
... After a significant number of CMIP6 production simula- tions were complete, it was determined that while conser- vative remapping was desirable for heat and water fluxes, it introduced issues in the wind-stress field ... See full document
9
Impact of assimilating sea ice concentration, sea ice thickness and snow depth in a coupled ocean–sea ice modelling system
... ESA Sea Ice Climate Change Initiative, Sea Ice Concentration Climate Data Record from the AMSR-E and AMSR-2 Instruments at 25 km Grid Spac- ing, version ... See full document
143
The initiation of Neoproterozoic “snowball” climates in CCSM3: the influence of paleocontinental configuration
... thick sea ice is assumed to have covered the entire surface of the oceans simultaneously with the continents being cov- ered by thick ice sheets during the glaciation events (“Stur- tian” at ∼ 720 ... See full document
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Sea-ice evaluation of NEMO-Nordic 1.0: a NEMO–LIM3.6-based ocean–sea-ice model setup for the North Sea and Baltic Sea
... the model has an overly thin snow ...while sea ice in the thickness range ...correct ice thickness distribution is clearly challenging and several things proba- bly affect the ...of ice ... See full document
459
On the discretization of the ice thickness distribution in the NEMO3.6-LIM3 global ocean–sea ice model
... Sea ice models as components of climate models are pri- mary tools to characterize climate variability at high lati- tudes (Holland et ...of sea ice models typically ranges from values as ... See full document
7
An ocean sea ice model study of the unprecedented Antarctic sea ice minimum in 2016
... s sea-ice and oceanic conditions to the 2016 sea ice minimum ( table 1 and fi gure 3 ) ...Antarctic sea ice, ...Ekman sea ice drift, and less sea ice ... See full document
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September Arctic sea ice minimum prediction – a skillful new statistical approach
... Arctic Ocean show also pronounced decadal to multidecadal variability (Zhang, ...Arctic sea ice is partially driven by AMO (Park and Latif, 2008; Lindsay et ...Arctic sea ice extent ... See full document
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