Descriptif ED1314-S2 - Historique des versions

Girault le 18 juillet 2018 à 13:00

2018-07-18T13:00:27Z

← Version précédente		Version du 18 juillet 2018 à 13:00
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-	This course serves at as introduction to utilizing the S-CAPAD platform (<http://webpublix.ipgp.fr/rech/scp>). It includes a general introduction to high-performance computing, and it covers the specifics of the S-CAPAD platform (in particular modules and job submissions), which are illustrated by a number of hands-on practicals.	+	This course serves at as introduction to utilizing the S-CAPAD platform (http://webpublix.ipgp.fr/rech/scp). It includes a general introduction to high-performance computing, and it covers the specifics of the S-CAPAD platform (in particular modules and job submissions), which are illustrated by a number of hands-on practicals.

Girault le 18 juillet 2018 à 13:00

2018-07-18T13:00:12Z

← Version précédente		Version du 18 juillet 2018 à 13:00
Ligne 1 :		Ligne 1 :
		+	This course serves at as introduction to utilizing the S-CAPAD platform (<http://webpublix.ipgp.fr/rech/scp>). It includes a general introduction to high-performance computing, and it covers the specifics of the S-CAPAD platform (in particular modules and job submissions), which are illustrated by a number of hands-on practicals.
		+
		+
	=Concepts généraux (2H)=		=Concepts généraux (2H)=

Narteau le 14 septembre 2014 à 11:30

2014-09-14T11:30:35Z

← Version précédente		Version du 14 septembre 2014 à 11:30
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-	~~An alluvial river is a river in which the bed and banks are made of mobile sediment. Alluvial rivers are self-formed, meaning that their shape result from the feedback between flow dynamics~~ and sediment transport. As a result, rivers build their own bed, selecting both their width and slope and developing planforms that can be meandering, or braiding. At a larger scale, rivers organize into a dendritical network called the drainage network. In this lecture, we will discuss some aspects of the interaction between flow and sediment transport with the goal to understand how a mechanism which operates at the scale of the fluid-~~grain interaction~~ (~~typically the centimeter and the second~~) ~~selects the shape of alluvial rivers and controls the growth of the drainage network.~~	+	=Concepts généraux (2H)=
-	In the second part of the lecture we will use recent publications on the flux of matter and dissolved elements to discuss the concept introduced in the first part of the lecture. The focus will be on the amazon basin and its different watershed of different sizes.	+
-	The objectives are to discuss the selection of papers. Groups of 2 PhD candidate will make first a short presentation of the papers to be discussed. The lecture should be critical and raise issues to be addressed in the futur. The outcome of this work could be the the redaction of a research proposal (~~2 pages~~) ~~on identified topics.~~	+	==Calcul scientifique et traitement de données==
		+	===Concepts====
		+	===Applications===
		+
		+	==Technologies dédiées au HPC==
		+	===Histoire===
		+	===Processeurs généralistes===
		+	===Accélérateurs GPU et MIC===
		+	===Réseaux d’interconnexion rapide===
		+
		+	==Architectures des solutions HPC
		+	===Grappes de calcul===
		+	===Evolutions futures===
		+
		+
		+
		+	=S-CAPAD et les travaux de calcul (2H30)=
		+
		+	==Connexion au supercalculateur - TP==
		+	===Client UNIX===
		+	===Client Windows===
		+
		+	==Gestion des données – TP==
		+	===Répertoires de connexion===
		+	===Espaces de travail globaux===
		+	===Espace de travail local===
		+
		+	==Soumission de travaux différés et interactifs – TP==
		+	===Principes des files d’attente===
		+	===Consultation des ressources disponibles et gestion de l’activité===
		+	===Mode différé===
		+	===Mode interactif
		+
		+	==Support technique et procédures==
		+	===Communauté utilisateurs===
		+	===Support système===
		+	===Support applicatif===
		+
		+
		+	=Environnement de développement (3H)=
		+
		+	==Modules d’environnement – TP==
		+
		+	==Compilateurs et bibliothèques – TP==
		+	===Compilateurs Intel et GNU===
		+	===Bibliothèques scientifiques===
		+
		+	==Introduction aux outils de développement – TP==
		+	===Debugger===
		+	===Profiler===
		+
		+	==Méthodologie d’optimisation des performances==

Prisca : Page créée avec « An alluvial river is a river in which the bed and banks are made of mobile sediment. Alluvial rivers are self-formed, meaning that their shape result from the feedback betwee… »

2014-01-10T09:59:42Z

Page créée avec « An alluvial river is a river in which the bed and banks are made of mobile sediment. Alluvial rivers are self-formed, meaning that their shape result from the feedback betwee… »

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An alluvial river is a river in which the bed and banks are made of mobile sediment. Alluvial rivers are self-formed, meaning that their shape result from the feedback between flow dynamics and sediment transport. As a result, rivers build their own bed, selecting both their width and slope and developing planforms that can be meandering, or braiding. At a larger scale, rivers organize into a dendritical network called the drainage network. In this lecture, we will discuss some aspects of the interaction between flow and sediment transport with the goal to understand how a mechanism which operates at the scale of the fluid-grain interaction (typically the centimeter and the second) selects the shape of alluvial rivers and controls the growth of the drainage network.
In the second part of the lecture we will use recent publications on the flux of matter and dissolved elements to discuss the concept introduced in the first part of the lecture. The focus will be on the amazon basin and its different watershed of different sizes.
The objectives are to discuss the selection of papers. Groups of 2 PhD candidate will make first a short presentation of the papers to be discussed. The lecture should be critical and raise issues to be addressed in the futur. The outcome of this work could be the the redaction of a research proposal (2 pages) on identified topics.