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% $Header: /u/gcmpack/manual/part6/seaice.tex,v 1.1 2004/08/30 19:25:41 edhill Exp $ |
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% $Name: $ |
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%%EH3 Copied from "MITgcm/pkg/seaice/seaice_description.tex" |
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%%EH3 which was written by Dimitris M. |
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\section{Sea Ice Package: ``seaice''} |
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\label{sec:pkg:seaice} |
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\begin{rawhtml} |
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<!-- CMIREDIR:package_seaice: --> |
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\end{rawhtml} |
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Package ``seaice'' provides a dynamic and thermodynamic interactive |
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sea-ice model. Sea-ice model thermodynamics are based on Hibler |
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\cite{hib80}, that is, a 2-category model that simulates ice thickness |
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and concentration. Snow is simulated as per Zhang et al. |
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\cite{zha98a}. Although recent years have seen an increased use of |
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multi-category thickness distribution sea-ice models for climate |
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studies, the Hibler 2-category ice model is still the most widely used |
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model and has resulted in realistic simulation of sea-ice variability |
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on regional and global scales. Being less complicated, compared to |
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multi-category models, the 2-category model permits easier application |
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of adjoint model optimization methods. |
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Note, however, that the Hibler 2-category model and its variants use a |
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so-called zero-layer thermodynamic model to estimate ice growth and |
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decay. The zero-layer thermodynamic model assumes that ice does not |
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store heat and, therefore, tends to exaggerate the seasonal |
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variability in ice thickness. This exaggeration can be significantly |
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reduced by using Semtner's \cite{sem76} three-layer thermodynamic |
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model that permits heat storage in ice. Recently, the three-layer |
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thermodynamic model has been reformulated by Winton \cite{win00}. The |
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reformulation improves model physics by representing the brine content |
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of the upper ice with a variable heat capacity. It also improves |
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model numerics and consumes less computer time and memory. The Winton |
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sea-ice thermodynamics have been ported to the MIT GCM; they currently |
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reside under pkg/thsice. At present pkg/thsice is not fully |
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compatible with pkg/seaice and with pkg/exf. But the eventual |
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objective is to have fully compatible and interchangeable |
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thermodynamic packages for sea-ice, so that it becomes possible to use |
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Hibler dynamics with Winton thermodyanmics. |
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The ice dynamics models that are most widely used for large-scale |
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climate studies are the viscous-plastic (VP) model \cite{hib79}, the |
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cavitating fluid (CF) model \cite{fla92}, and the |
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elastic-viscous-plastic (EVP) model \cite{hun97}. Compared to the VP |
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model, the CF model does not allow ice shear in calculating ice |
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motion, stress, and deformation. EVP models approximate VP by adding |
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an elastic term to the equations for easier adaptation to parallel |
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computers. Because of its higher accuracy in plastic solution and |
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relatively simpler formulation, compared to the EVP model, we decided |
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to use the VP model as the dynamic component of our ice model. To do |
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this we extended the alternating-direction-implicit (ADI) method of |
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Zhang and Rothrock \cite{zha00} for use in a parallel configuration. |
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The sea ice model requires the following input fields: 10-m winds, 2-m |
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air temperature and specific humidity, downward longwave and shortwave |
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radiations, precipitation, evaporation, and river and glacier runoff. |
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The sea ice model also requires surface temperature from the ocean |
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model and third level horizontal velocity which is used as a proxy for |
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surface geostrophic velocity. Output fields are surface wind stress, |
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evaporation minus precipitation minus runoff, net surface heat flux, |
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and net shortwave flux. The sea-ice model is global: in ice-free |
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regions bulk formulae are used to estimate oceanic forcing from the |
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atmospheric fields. |
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%\subsection{Package Reference} |
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