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Journal ArticleDOI

Impact of uncertainties in the horizontal density gradient upon low resolution global ocean modelling

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TLDR
In this article, it is shown that unresolved scales represent a major source of uncertainties in the computation of the large-scale horizontal density gradient from the large scale temperature and salinity fields, and that the effect of these uncertainties can be simulated using random processes to represent unresolved temperature fluctuations.
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This article is published in Ocean Modelling.The article was published on 2013-06-01. It has received 70 citations till now. The article focuses on the topics: Temperature salinity diagrams & Geostrophic wind.

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Toward a stochastic parameterization of ocean mesoscale eddies

TL;DR: In this paper, a stochastic parameterization of ocean mesoscale eddies is constructed in order to account for the fluctuations in subgrid transport and to represent upscale turbulent cascades.
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Challenges and Prospects in Ocean Circulation Models

B. Fox-Kemper, +35 more
TL;DR: In this article, the authors revisit the challenges and prospects for ocean circulation models following Griffies et al. (2010), and summarize new developments in ocean modeling, including: how new and existing observations can be used, what modeling challenges remain, and how simulations can also be used to support observations.

Coupled Data Assimilation for Integrated Earth System Analysis and Prediction: Goals, Challenges, and Recommendations

TL;DR: In this paper, the authors identify fundamental issues for coupled data assimilation (CDA), such as gaps in science and limitations in forecasting systems, in order to provide guidance to the World Meteorological Organization (WMO) on how to facilitate more rapid progress internationally.
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Scale-aware deterministic and stochastic parametrizations of eddy-mean flow interaction

TL;DR: In this paper, the authors proposed an eddy parametrization based on a non-Newtonian stress which depends on the partially resolved scales and their variability, and tested two versions of the parameter, one deterministic and one stochastic, at coarse and eddy-permitting resolutions in a double gyre quasi-geostrophic model.
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Will high-resolution global ocean models benefit coupled predictions on short-range to climate timescales?

TL;DR: In this article, the benefits of increased ocean resolution in global coupled models, where the ocean component explicitly represents transient mesoscale eddies and narrow boundary currents, are discussed and a discussion of what processes can presently be parameterized in coupled models with coarse resolution non-eddying ocean models, and where parameterizations may fall short.
References
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Journal ArticleDOI

Sequential data assimilation with a nonlinear quasi-geostrophic model using Monte Carlo methods to forecast error statistics

TL;DR: In this article, a new sequential data assimilation method is proposed based on Monte Carlo methods, a better alternative than solving the traditional and computationally extremely demanding approximate error covariance equation used in the extended Kalman filter.
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The global climatology of an interannually varying air–sea flux data set

TL;DR: The air-sea fluxes of momentum, heat, freshwater and their components have been computed globally from 1948 to 2006 at frequencies ranging from 6-hourly to monthly as mentioned in this paper.
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Stochastic representation of model uncertainties in the ECMWF ensemble prediction system

TL;DR: In this paper, a stochastic representation of random error associated with parametrized physical processes is described, and its impact in the European Centre for Medium-Range Weather Forecasts Ensemble Prediction System (ECMWF EPS) is discussed.
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Variability of the Tropical Atlantic Ocean Simulated by a General Circulation Model with Two Different Mixed-Layer Physics

TL;DR: In this article, a 1.5 turbulence closure model in an ocean general circulation model of the equatorial Atlantic is presented, where the eddy viscosity and diffusivity involved in the vertical mixing are defined as the product of a characteristic turbulent velocity and a characteristic mixing length.
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