LEGI - UMR 5519

09/01/2020 - Eletta Negretti
La prédiction de l’évolution du climat dépend de notre compréhension de la dynamique des océans sur une grande variété d’échelles en interaction en temps et l’espace. Les (...)

05/07/2018 - Claudine Charrondière
Le refroidissement des couches d’air en surface, dû à un bilan d’énergie en surface négatif, est à l’origine d’écoulements catabatiques, souvent la nuit. Modélisés sans (...)

14/06/2018 - Bruno Voisin
Rotation alters fundamentally the wake of a moving body, or the flow past a fixed obstacle : inertial waves are generated and vortex shedding is hindered. We present a (...)

31/05/2018 - Maurizio Brocchini DICEA, Università Politecnica delle Marche, Ancona, Italy
The role of wave forcing on the main hydro-morphological dynamics evolving in the shallow waters of the (...)

16/05/2018 - Hai Yen Tran
This study focuses on the feasibility of a combined model that includes longshore sediment transport effects in a cross-shore shoreline evolution model. Longshore (...)

03/05/2018 - Guoqing Han K118 12h15
Abstract The sea surface temperature (SST) anomaly in the Mozambique Channel is revealed by high resolution satellite remote sensing data . The data analysis (...)

26/04/2018 - Yeulwoo Kim
Wave-driven sediment transport is one of the key drivers of beach morphodyanmics. However, a comprehensive understanding of that has not been achieved due to many (...)

12/04/2018 - Garcìa Molina Cruz
Motivated by field measurements and numerical modeling of the interaction of the Antarctic Circumpolar Current (ACC) with rough topography in the Southern Ocean (...)

15/03/2018 - Cédric Lachaud (IGE)
The brittle deformation of ice has important environmental applications, mostly regarding to our understanding at the future evolution of ice sheet and sea ice. (...)

Maria Chiara De Falco - 22/02/2018
The propagation of gravity currents develops generally over complex boundaries in several natural fields. In particular, density currents can propagate up a (...)