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Physically Consistent Eddy-resolving State Estimation and Prediction of the Coupled Pan-Arctic Climate System at Daily to Interannual Time Scales Using the Regional Arctic Climate Model (RACM)

TLDR
In this article, the authors use the Regional Arctic System Model (RASM) to extend the Navy sea ice predictive capability beyond the current forecasts of up to 7-day (provided by the Arctic Cap Nowcast/Forecast System (ACNFS) at NRL), to seasonal and up to decadal climate projections.
Abstract
: This project targets some of the key requirements in the Navy Arctic Roadmap 2014-2030 and in the 2014 Implementation Plan for the National Strategy for the Arctic Region, regarding the need for advanced modeling capabilities for operational forecasting and strategic climate predictions through 2030. The proposed research leverages ongoing developments of the state-of-the-art Regional Arctic System Model (RASM, previously called Regional Arctic Climate Model - RACM) through a multiinstitutional program supported by the Department of Energy Regional and Global Climate Modeling (DOE/RGCM) program and two ongoing complementary projects. This project is aimed at improved modeling of the atmosphere-ice-ocean interface to advance representation of the past and present state of the Arctic Climate System and prediction of its future states at time scales from daily (operational) through seasonal, interannual, and up to decadal (tactical). We use the Regional Arctic System Model (RASM) to extend the Navy sea ice predictive capability beyond the current forecasts of up to 7-day (provided by the Arctic Cap Nowcast/Forecast System (ACNFS) at NRL), to seasonal and up to decadal climate projections. Three main objectives are to (i) advance understanding and model representation of critical physical processes and feedbacks of importance to sea ice thickness and area distribution using a combination of forward modeling and state estimation techniques, (ii) investigate the relation between the upperocean heat content and sea ice volume change and its potential feedback in amplifying ice melt, (iii) upgrade RASM with the above improvements to advance both operational and tactical prediction of arctic climate using a single model.

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Citations
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Incorporation of a physically-based melt pond scheme into the sea ice component of a climate model

TL;DR: In this article, the authors developed a melt pond evolution theory and incorporated this theory into the Los Alamos CICE sea ice model, which has required us to include the refreezing of melt ponds.

Contrasts in Sea Ice Deformation and Production In the Arctic Seasonal and Perennial Ice Zones

TL;DR: In this paper, the authors compared the sea ice deformation and production regionally and in the seasonal (SIZ) and perennial (PIZ) ice zones, and provided 3-day estimates of these quantities within Lagrangian elements.
References
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Journal ArticleDOI

An Elastic–Viscous–Plastic Model for Sea Ice Dynamics

TL;DR: In this article, the authors developed and tested two separate methods for sea ice dynamics, and showed that the viscous-plastic rheology can be represented by a symmetric, negative definite matrix operator, leading to a faster and better behaved preconditioned conjugate gradient method.

An elastic-viscous-plastic model for sea ice dynamics

TL;DR: In this paper, the authors proposed an explicit discretization of the elastic wave mechanism, which allows the elastic-viscous-plastic model to capture the ice response to variations in the imposed stress more accurately.
Journal ArticleDOI

A Multiscale Nonhydrostatic Atmospheric Model Using Centroidal Voronoi Tesselations and C-Grid Staggering

TL;DR: The formulation of a fully compressible nonhydrostatic atmospheric model called the Model for Prediction Across Scales–Atmosphere (MPAS-A) is described, using centroidal Voronoi meshes and a C-grid staggering of the prognostic variables to incorporate a split-explicit time-integration technique used in many existing meso- and cloud-scale models.
Journal ArticleDOI

A unified approach to energy conservation and potential vorticity dynamics for arbitrarily-structured C-grids

TL;DR: A numerical scheme applicable to arbitrarily-structured C-grids is presented for the nonlinear shallow-water equations, using the vector-invariant form of the momentum equation to guarantee that mass, velocity and potential vorticity evolve in a consistent and compatible manner.
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