A Reformulated Three-Layer Sea Ice Model

By M. Winton. 2000

469 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/a590fc2fa83859e138c8b0e7120e27161f7b8ded

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In Atmospheric Science

Citations in the corpus

System Design and Evaluation of Coupled Ensemble Data Assimilation for Global Oceanic Climate Studies (2007, methodology): “The elastic–viscous–plastic technique (Hunke and Dukowicz 1997) is used to calculate the internal stresses of the ice, and the thermodynamics follows a modified Semtner three-layer scheme (Winton 2000).”
Parameterizing the fresh-water flux from land ice to ocean with interactive icebergs in a coupled climate model (2010, background): “The sea ice simulator (SIS) has multiple ice thickness categories and comprises the three-layer-thermodynamics of Winton (2000) including a prognostic snow cover.”
The GFDL CM3 Coupled Climate Model: Characteristics of the Ocean and Sea Ice Simulations (2011, background): “1, as documented in Delworth et al. (2006) and Winton (2000), and it uses the same horizontal grid arrangement of the ocean model.”
SODA3: A New Ocean Climate Reanalysis (2018, methodology): “The sea ice model uses the GFDL Sea Ice Simulator dynamics and thermodynamics of Winton (2000) on the same numerical grid.”
The Role of Bottom Vortex Stretching on the Path of the North Atlantic Western Boundary Current and on the Northern Recirculation Gyre (2007, methodology): “We coupled a two-dimensional global atmospheric EBM with hydrological cycle to a global OGCM (GFDL MOM4; Griffies et al. 2004) and a slab sea ice model (Winton 2000).”
Climate Models: An Assessment of Strengths and Limitations (2008, background): “The GFDL climate models continue to use this but also include the interactions between brine content and heat capacity (Winton 2000).”
The ocean’s role in setting the mean position of the Inter-Tropical Convergence Zone (2013, methodology): “, the latitude of maximum zonal mean precipitation used by Xian and Miller (2008), the zonal average of the latitude of maximum precipitation at each longitude as in Waliser and Gautier (1993) or the precipitation centroid used by Frierson and Hwang (2012)—place the annual mean ITCZ north of the Equ”
Equilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean Response (2008, background): “The dynamic part of the sea ice component employs an elastic–viscous–plastic ice rheology, and predicts velocity of the ice pack and the area as described in Winton (2000).”
An assessment of oceanic variability for 1960–2010 from the GFDL ensemble coupled data assimilation (2013, methodology): “The elastic-viscous-plastic technique (Hunke and Dukowicz 1997) is used to calculate ice internal stress, and the thermodynamics is a modified Semtner three-layer scheme (Winton 2000).”
Volcanic signals in oceans (2009, methodology): “It uses the elastic-viscousplastic rheology to calculate ice internal stresses, and a modified Semtner three-layer scheme for thermodynamics [ Winton, 2000 ].”
GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics (2006, methodology): “For details see Winton (2000).”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “SIS2.”
Assessment of Twentieth-Century Regional Surface Temperature Trends using the GFDL CM2 Coupled Models (2006, methodology): “The model uses the elastic-viscous-plastic rheology to calculate ice internal stresses, and a modified Semtner three-layer scheme for thermodynamics (Winton 2000).”
The global ocean is an ecosystem: simulating marine life and fisheries (2015, methodology): “The COBALT model captures large-scale patterns in carbon flow through the planktonic food web, and was implemented in the GFDL modular ocean model version 4p1 (Griffies, 2012) with sea-ice dynamics as described by Winton (2000).”
The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3 (2011, background): “1 (Delworth et al. 2006; Winton 2000) except for some parameter resetting made possible by improved realism in the CM3 climate in regions of sea ice.”
Seasonal Prediction of Arctic Sea Ice Extent from a Coupled Dynamical Forecast System (2013, methodology): “The sea ice dynamics is based on Hunke and Dukowicz (1997) using the elastic–viscous– plastic technique to calculate ice internal stress, while the sea ice thermodynamics is based on Winton (2000).”
Evolution of the Global Coupled Climate Response to Arctic Sea Ice Loss during 1990–2090 and Its Contribution to Climate Change (2018, background): “Internal climate variability may also have contributed to sea ice loss (e.g., Mahajan et al. 2011; Day et al. 2012; Yeager et al. 2015; Zhang 2015; Ding et al. 2017; Lee et al. 2017; Li et al. 2017, 2018).”
On the formulation of sea-ice models. Part 1: Effects of different solver implementations and parameterizations (2010, methodology): “…2nd-order advection216 scheme with a SuperBee flux limiter (Roe, 1985) is used in this study to ad-217 vect all sea-ice-related quantities of the Winton (2000) thermodynamic model.218 Because of the non-linearity of the advection scheme, care must be taken in219 advecting these quantities: when…”