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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><a href="uid8.html&#10;&#9;&#9;  ">Data assimilation and inverse modeling</a></li><li class="tdmActPage"><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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	    2013</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">Satellite acquisitions and image assimilation</h3>
        <p>In geosciences, the issue of coupling data, in particular satellite
acquisitions, and models is extensively studied for meteorology,
oceanography, chemistry-transport and land surface models. However,
satellite images are mostly assimilated on a point-wise basis. Three major approaches
arise if taking into account the spatial structures, whose displacement is
visualized on image sequences:</p>
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            <p class="notaparagraph"><a name="uid15"> </a>Image approach. Image assimilation allows the extraction of features
from image sequences, for instance motion field or structures' trajectory. A model of the dynamics is
considered (obtained by simplification of a geophysical model such as Navier-Stokes equations). An
observation operator is defined to express the links between the model state
and the pixels values. In the simplest case, the pixel value corresponds to
one coordinate of the model state and the observation operator is reduced to a
projection. However, in most cases, this operator is highly complex, implicit
and non-linear. Data assimilation techniques are developed to control the
initial state or the whole assimilation window. Image assimilation is also
applied to learn reduced models from image data and estimate a reliable and
small-size reconstruction of the dynamics, which is observed on the
sequence.</p>
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            <p class="notaparagraph"><a name="uid16"> </a>Model approach. Image assimilation is used to control an environmental
model and obtain improved forecasts. In order to take into account the
spatial and temporal coherency of structures, specific image characteristics
are considered and dedicated norms and observation error covariances are
defined.</p>
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            <p class="notaparagraph"><a name="uid17"> </a>Correcting a model. Another topic, mainly described for meteorology
in the literature, concerns the location of structures. How to force
the existence and to correct the location of structures in the model state
using image information? Most of the operational meteorological forecasting
institutes, such as MétéoFrance, UK-met, KNMI (in Netherlands), ZAMG (in
Austria) and Met-No (in Norway), study this issue because operational
forecasters often modify their forecasts based on visual comparisons between the
model outputs and the structures displayed on satellite images.</p>
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