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      <div class="TdmEntry">Overall Objectives<ul><li><a href="./uid3.html">Clime in short</a></li></ul></div>
      <div class="TdmEntry">Research Program<ul><li class="tdmActPage"><a href="uid8.html&#10;&#9;&#9;  ">Data assimilation and inverse modeling</a></li><li><a href="uid14.html&#10;&#9;&#9;  ">Satellite acquisitions and image assimilation</a></li><li><a href="uid18.html&#10;&#9;&#9;  ">Software chains for environmental
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        Data assimilation library: Verdandi
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        Polyphemus
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	    Raweb 
	    2014</a> | <a href="http://www.inria.fr/en/teams/clime">Presentation of the Project-Team CLIME</a> | <a href="http://www-rocq.inria.fr/clime/index.en.html">CLIME Web Site
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        <h2>Section: 
      Research Program</h2>
        <h3 class="titre3">Data assimilation and inverse modeling</h3>
        <p>This activity is one major concern of environmental
sciences. It matches up the setting and the use of data assimilation methods,
for instance variational methods (such as the 4D-Var method). An emerging issue lies in the
propagation of uncertainties by models, notably through ensemble forecasting
methods.</p>
        <p>Although modeling is not part of the scientific objectives of Clime, the
project-team has complete access to models through collaborations with CEREA
(Centre d'Enseignement et de Recherche en Environnement Atmosphérique, École des Ponts ParisTech): the models from
Polyphemus (pollution forecasting from local to regional scales) and
Code_Saturne (urban scale). In regard to other modeling domains, such as
meteorology and oceanography, Clime
accesses models through co-operation with LOCEAN (Laboratoire d'OCEANographie
et du climat, UPMC).</p>
        <p>The research activities of Clime tackle scientific issues such as:</p>
        <ul>
          <li>
            <p class="notaparagraph"><a name="uid9"> </a>Within a family of models (differing by their physical formulations and
numerical approximations), which is the optimal model for a given set of
observations?</p>
          </li>
          <li>
            <p class="notaparagraph"><a name="uid10"> </a>How to reduce dimensionality of problems by Galerkin projection of
equations on subspaces? How to define these subspaces in order to keep the
main properties of systems?</p>
          </li>
          <li>
            <p class="notaparagraph"><a name="uid11"> </a>How to assess the quality of a forecast and its uncertainty? How do data quality, missing
data, data obtained from sub-optimal locations, affect the forecast? How to
better include information on uncertainties (of data, of models) within the
data assimilation system?</p>
          </li>
          <li>
            <p class="notaparagraph"><a name="uid12"> </a>How to make a forecast (and a better forecast!) by using several models
corresponding to different physical formulations? It also raises the
question: how should data be assimilated in this context?</p>
          </li>
          <li>
            <p class="notaparagraph"><a name="uid13"> </a>Which observational network should be set up to perform a better
forecast, while taking into account additional criteria such as observation
cost? What are the optimal location, type and mode of deployment of sensors?
How should trajectories of mobile sensors be operated, while the
studied phenomenon is evolving in time? This issue is usually referred as
“network design”.</p>
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