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            <Subtitle>The  Sciences &amp;amp; Technologies Update  collection   publishes works in French or English, taking stock of recent progress in various scientific and technological fields. It is geared towards scientists in the fields concerned. It follows on from the following collections: Science update (Inra).</Subtitle>
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        <BiographicalNote>&lt;p&gt;Pietro Bernardara est ingénieur de recherche au Laboratoire national d’hydraulique et environnement à Chatou (EDF, Recherche et développement). Après une thèse sur la modélisation spatio-temporelle des champs pluvieux à l’aide d’outils multifractals, il a effectué un post-doctorat au Cemagref et au Cereve de 2004 à 2006, dans le but de faire le lien entre hydrologie et théorie multifractale.&lt;/p&gt;</BiographicalNote>
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        <BiographicalNote language="fre">&lt;p&gt;Éric Sauquet est hydrologue et chercheur à INRAE (UR Riverly). Il est directeur du métaprogramme CLIMAE.&lt;/p&gt;</BiographicalNote>
        <BiographicalNote language="eng">&lt;p&gt;Éric Sauquet is a hydrologist and researcher at INRAE (UR Riverly). He is director of the CLIMAE metaprogram.&lt;/p&gt;</BiographicalNote>
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        <BiographicalNote>&lt;p&gt;Daniel Schertzer, ingénieur en chef au Cereve à l’École nationale des ponts et chaussées (ENPC) à Marne-La-Vallée, est l’un des spécialistes internationaux reconnus de l’analyse multifractale.&lt;/p&gt;</BiographicalNote>
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        <BiographicalNote>&lt;p&gt;Ioulia Tchiguirinskaia mathématicienne chargée de recherche au Cereve (ENPC), a travaillé sur l’analyse multifractale de nombreuses séries environnementales.&lt;/p&gt;</BiographicalNote>
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        <Text language="fre">&lt;p&gt;&lt;b&gt;Cet ouvrage en impression à la demande sera envoyé sous 3 semaines environ (France métropolitaine) et dans un colis séparé en cas de commande avec un autre livre papier.&lt;/b&gt;&lt;/p&gt;&lt;p&gt;Cet ouvrage propose une procédure simplifiée pour réaliser une analyse de séries hydrologiques dans un cadre multifractal. Après un rappel de la théorie des multifractales, il décrit un modèle permettant d’identifier les propriétés d’invariance d’échelle, et présente des exemples d’application à des séries temporelles de pluie et de débit. Il intéressera les enseignants et chercheurs de la discipline tant au niveau national qu’international.&lt;/p&gt;&lt;p&gt;&amp;nbsp;&lt;/p&gt;&lt;b&gt;The English version of this book,&amp;nbsp;&lt;i&gt;&lt;a href="https://www.quae.com/produit/1017/9782759213993/multifractal-analysis-in-hydrology" target="_blank"&gt;Multifractal analysis in hydrology&lt;/a&gt;&lt;/i&gt;, is available on our website.&lt;/b&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;b&gt;La version anglaise de ce titre, &lt;i&gt;&lt;a href="https://www.quae.com/produit/1017/9782759213993/multifractal-analysis-in-hydrology" target="_blank"&gt;Multifractal analysis in hydrology&lt;/a&gt;&lt;/i&gt;, est disponible sur notre site.&lt;/b&gt;&lt;/p&gt;</Text>
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        <Text>Cet ouvrage propose une procédure simplifiée pour réaliser une analyse de séries hydrologiques dans un cadre multifractal. Des exemples d’application à des séries temporelles de pluie et de débit sont présentés.</Text>
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        <Text>&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Introduction&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 4pt"&gt;&lt;strong&gt;&amp;#160;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Chapitre 1. La théorie multifractale&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 4pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Comment observer un phénomène à différentes échelles ?&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Le rapport d'échelle &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Les observations et les échelles d'un processus hydrologique &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Les singularités &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Une description statistique des processus multifractals &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La fonction codimension &lt;em&gt;c(y)&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La fonction des moments statistiques &lt;em&gt;K(q)&lt;/em&gt; &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Propriétés générales des multifractals &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Multifractales et extrêmes &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La divergence des moments &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Effet de la taille de l'échantillon &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Diagnostic sur la présence de valeurs extrêmes&lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Présentation des modèles de cascades multiplicatives &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Description générale &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Propriétés des séries générées par une cascade multiplicative &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Commentaire sur les champs conservatifs et non-conservatifs&lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Le modèle multifractal universel &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Commentaire sur l'estimation des paramètres multifractals universels &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Le modèle multifractal universel et les extrêmes&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Chapitre 2. 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        <Text>Cet ouvrage propose une procédure simplifiée pour réaliser une analyse de séries hydrologiques dans un cadre multifractal. Des exemples d’application à des séries temporelles de pluie et de débit sont présentés.</Text>
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        <Text>&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Introduction&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 4pt"&gt;&lt;strong&gt;&amp;#160;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Chapitre 1. La théorie multifractale&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 4pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Comment observer un phénomène à différentes échelles ?&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Le rapport d'échelle &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Les observations et les échelles d'un processus hydrologique &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Les singularités &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Une description statistique des processus multifractals &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La fonction codimension &lt;em&gt;c(y)&lt;/em&gt;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La fonction des moments statistiques &lt;em&gt;K(q)&lt;/em&gt; &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Propriétés générales des multifractals &lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Multifractales et extrêmes &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;La divergence des moments &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Effet de la taille de l'échantillon &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Diagnostic sur la présence de valeurs extrêmes&lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Présentation des modèles de cascades multiplicatives &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Description générale &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Propriétés des séries générées par une cascade multiplicative &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Commentaire sur les champs conservatifs et non-conservatifs&lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Le modèle multifractal universel &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Commentaire sur l'estimation des paramètres multifractals universels &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Le modèle multifractal universel et les extrêmes&lt;/span&gt;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Chapitre 2. Application des multifractales à des chroniques de pluie et de débit &lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 5pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Données&lt;/span&gt;&lt;/div&gt;&lt;div style="LINE-HEIGHT: 3pt"&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Analyse multifractale de séries de pluie et de débit &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Analyse spectrale &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Analyse des lois d'échelle des moments &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Calage des paramètres multifractals universels &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Commentaire sur les valeurs extrêmes &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Conclusion &lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Remerciements &lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Annexes&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Intégration et différenciation fractionnaire &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&lt;span style="FONT-SIZE: 8pt"&gt;&amp;#160;Table des notations utilisées &lt;/span&gt;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Références bibliographiques &lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&lt;strong&gt;&lt;span style="FONT-SIZE: 8pt"&gt;Liste des auteurs &lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div&gt;&amp;#160;&lt;/div&gt;&lt;div style="MARGIN: 0cm 0cm 0pt 42.55pt"&gt;&amp;#160;&lt;/div&gt;</Text>
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