about
P286
Towards multi-resolution global climate modeling with ECHAM6–FESOM. Part I: model formulation and mean climateAn assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part I: Sea ice and solid freshwaterAn assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part II: Liquid freshwaterAn assessment of the Arctic Ocean in a suite of interannual CORE-II simulations. Part III: Hydrography and fluxesThe Relative Influence of Atmospheric and Oceanic Model Resolution on the Circulation of the North Atlantic Ocean in a Coupled Climate ModelOcean Modeling on a Mesh With Resolution Following the Local Rossby RadiusNorth Atlantic simulations in Coordinated Ocean-ice Reference Experiments phase II (CORE-II). Part II: Inter-annual to decadal variabilityAn assessment of Antarctic Circumpolar Current and Southern Ocean meridional overturning circulation during 1958–2007 in a suite of interannual CORE-II simulationsAn assessment of Southern Ocean water masses and sea ice during 1988–2007 in a suite of interannual CORE-II simulationsAn assessment of global and regional sea level for years 1993–2007 in a suite of interannual CORE-II simulationsNorth Atlantic simulations in Coordinated Ocean-ice Reference Experiments phase II (CORE-II). Part I: Mean statesEvaluation of a Finite-Element Sea-Ice Ocean Model (FESOM) set-up to study the interannual to decadal variability in the deep-water formation ratesEnhanced cross-shelf exchange by tides in the western Ross SeaOverflow dynamics and bottom water formation in the western Ross Sea: Influence of tidesComparison of the Effect of Parameterized Eddy Fluxes of Thickness and Potential VorticityA finite-element ocean model: principles and evaluationNorth and equatorial Pacific Ocean circulation in the CORE-II hindcast simulationsOcean circulation and sea ice distribution in a finite element global sea ice–ocean modelDesigning variable ocean model resolution based on the observed ocean variabilityInfluence of a Salt Plume Parameterization in a Coupled Climate ModelArctic Sea Ice Decline Significantly Contributed to the Unprecedented Liquid Freshwater Accumulation in the Beaufort Gyre of the Arctic OceanThe Benefits of Global High Resolution for Climate Simulation: Process Understanding and the Enabling of Stakeholder Decisions at the Regional ScaleRhines scale and spectra of the β-plane turbulence with bottom dragNonuniversal features of forced two-dimensional turbulence in the energy rangeMean force on a small sphere in a sound field in a viscous fluidForced two-dimensional turbulence in spectral and physical spaceExperiments on free decay of quasi-two-dimensional turbulent flows
P50
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P50
description
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
Sergey Danilov
@ast
Sergey Danilov
@en
Sergey Danilov
@es
Sergey Danilov
@nl
type
label
Sergey Danilov
@ast
Sergey Danilov
@en
Sergey Danilov
@es
Sergey Danilov
@nl
prefLabel
Sergey Danilov
@ast
Sergey Danilov
@en
Sergey Danilov
@es
Sergey Danilov
@nl
P106
P31
P496
0000-0001-8098-182X