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Leçon Particularités de la langue latine quelques phonèmes spécifiques c k e g g i j En latin i est semi voyelle semi consonne Correspond deux sons i i et j dictionnaires gardent la double graphie i pour le i voyelle et j pour le i consonne graphème –qu kw s en position intervocalique reste sourd s u v u également semi voyelle semi consonne u u ou et w y y pas de sons nasalisés en latin une langue déclinaison repérer qui n a jamais appris de langue déclinaison expliquer le principe des langues flexionnelle langues reposant sur système fonctionnel Expliciter les notions de radical de thème de désinence étude des cas présents en latin et de leurs valeurs Insister sur la notion de valeur Savoir construire des hypothèses sur les cas Distribuer et travailler sur le VADEMECUM de l analyse syntaxique icon
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Collège - Lycée

Leçon Particularités de la langue latine quelques phonèmes spécifiques c k e g g i j En latin i est semi voyelle semi consonne Correspond deux sons i i et j dictionnaires gardent la double graphie i pour le i voyelle et j pour le i consonne graphème –qu kw s en position intervocalique reste sourd s u v u également semi voyelle semi consonne u u ou et w y y pas de sons nasalisés en latin une langue déclinaison repérer qui n'a jamais appris de langue déclinaison expliquer le principe des langues flexionnelle langues reposant sur système fonctionnel Expliciter les notions de radical de thème de désinence étude des cas présents en latin et de leurs valeurs Insister sur la notion de valeur Savoir construire des hypothèses sur les cas Distribuer et travailler sur le VADEMECUM de l'analyse syntaxique

Marie-Anne Bernolle
Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea icon
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Educație

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru
Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea icon
Category

Documente

Educație

Tsunami detection in the ionosphere by Juliette Artru Caltech Pasadena USA Philippe Lognonné Giovanni Occhipinti François Crespon Raphael Garcia IPGP Paris France Eric Jeansou Noveltis Toulouse France and Makoto Murakami GSI Tsukuba Japan Introduction Tsunamis are surface gravity waves that propagate for great distances in the oceans usually triggered by earthquakes or landslides In the open ocean their long wavelengths typically km long periods minutes and small amplitudes a few to cm for the gigantic event of December make their detection very challenging even with the deployment of GPS buoy systems Gonzalez et al Recently satellite altimetry has proved to be capable of measuring the sea

Juliette Artru