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<h2><b>For current research projects that I am involved in see <a id=link href="http://gica.exa.unne.edu.ar/research.php"> Group Research </b></h2>
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<h1 align="center"> ASDE - 4DVar </h1>
For several years we have been developing a  four-dimensional variational assimilation system (Pulido and Thuburn, QJ <a id=link href="http://gica.exa.unne.edu.ar/publi/pt_qj05.pdf">2005</a>, <a id=link href="http://gica.exa.unne.edu.ar/publi/pt_qj06.pdf">2006</a>) based on the middle atmosphere dynamical model of the University of Reading (Thuburn MWR, <a id=link href="http://ams.allenpress.com/perlserv/?request=get-document&amp;doi=10.1175%2F1520-0493%281997%29125%3C2328%3AAPBSWM%3E2.0.CO%3B2"> 1997</a>; Andrews, PhD Thesis Univ. of Reading, 2001). The model has a hexagonal-icosahedral grid with isentropic levels as the vertical coordinate. The system is also composed by an adjoint model (i.e. a full adjoint of the tangent linear model) and an optimization module based on conjugate gradients.

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We called it ASDE (Assimilation System for Drag Estimation) since gravity wave drag/parameter estimation was the first application of the system. 
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<img src="http://gica.exa.unne.edu.ar/imagenes/dragx02_07.png"><br>

Zonal gravity wave drag estimated by ASDE in August 2002 using Met Office analysis
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<b>Please do not hesitate to contact me to pulido <i> at </i> exa.unne.edu.ar if you are interested in the source codes of the assimilation system. </b> 
