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4 <title>Unresolved process parameterization.</title>
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75 <td width="11" valign="top" bgcolor="#C0E7B4"><span class="style11"><img src="/images/spacer.gif" input title="" width="10" height="30"></span></td>
76 <td colspan="3" valign="middle" bgcolor="#C0E7B4"><p align="center"><span class="style34">Representation of sub-grid-scale eddy and mixed-layer processes</span></p></td>
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137 <head>
138 <title>Unresolved process parameterization.</title>
139 <link rel="shortcut icon" href="/ecco.ico" >
140 </head>
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142 <!-- <h1>Representation of sub-grid-scale eddy and mixed-layer processes.</h1>
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144 <h4>People</h4>
145 <A href="mailto:dfer@mit.edu"> David Ferreira</A>,<br>
146 <A href="mailto:raffaele@mit.edu"> Raffaele Ferrari</A>,<br>
147 <A href="mailto:baylor@mit.edu"> Baylor Fox-Kemper</A>, <br>
148 <A href="mailto:jmarsh@mit.edu">John Marshall</A> <br>
149 and <A href="mailto:cnh@mit.edu">Chris Hill</A>
150
151
152 <h4>Project Description</h4>
153 Eddying solutions from ECCO2 experiments are being used by members of the
154 <a href=
155 "http://www.usclivar.org/Newsletter/VariationsV4N1/ClivarCPT_Emilie.pdf">
156 Climate Process Team on Eddy Mixed Layer Interactions</a>
157 to diagnose fluxes of heat and buoyancy
158 due to eddy processes in the global oceans. Results (such as
159 the diagnosed eddy heat and temperature transports shown in the figures below)
160 are being compared against observations, theoretical models and against very
161 high-resolution process models. This work is leading to a more complete
162 understanding of the role ocean eddies and mixed-layer processes play in
163 setting the global ocean state. <br>
164 <A href="ZonalMeanEddyFluxes.jpeg"
165 alt="Zonal average of the meridional eddy flux of temperature diagnosed from five years of the ECCO2 1/8th degree, isotropic grid MITgcm simulation.">
166 <img src="ZonalMeanEddyFluxes.jpeg" width=600>
167 </A>
168 <br>
169 Zonal average of the meridional eddy flux of temperature diagnosed from two years of the ECCO2 1/8th degree, isotropic grid
170 MITgcm simulation.
171 <br>
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173 <br>
174 <A href="Eddy_HT.jpeg"
175 alt="Vertically and zonally integrated heat flux diagnosed from two years of the ECCO2 1/8th degree, isotropic grid
176 MITgcm simulation.">
177 <img src="Eddy_HT.jpeg" width=600>
178 </A>
179 <br>
180 Vertically and zonally integrated heat flux for the full water column and for the upper 200m. Diagnosed from two years of the ECCO2 1/8th degree, isotropic grid MITgcm simulation.
181 <br>
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183 <br>
184 <A href="OHT_May02_Apr04.jpeg"
185 alt="Total poleward heat transport. Diagnosed from two years of the ECCO2 1/8th degree, isotropic grid MITgcm simulation.">
186 <img src="OHT_May02_Apr04.jpeg" width=600>
187 </A>
188 <br>
189 Total poleward heat transport diagnosed from two years of the ECCO2 1/8th degree, isotropic grid MITgcm simulation (red line) and observational estimates with associated errors (black lines).
190 <br>
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192 <br>
193 The application of ECCO2 high-resolution solutions can be seen in this <a href="CPT-EMILIE-2006.pdf">climate process team presentation</a> in which eddy transports from the explcitly
194 resolved model are compared against existing and new parameterizations.
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