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2-D models of tide currents are the most used to obtain a description of the circulation in coastal zones, from initial conditions in this area, and limit conditions (depth water). The lack of precision in open limits and the approximation of mathema
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_________7::04b818d91df84ece10125f708ff0a837
https://archimer.ifremer.fr/doc/00000/1261/
https://archimer.ifremer.fr/doc/00000/1261/
Present-day understanding of rill dynamics is hampered by a lack of detailed data on velocity distributions in rills. The latter are difficult to collect with traditional techniques due to the very low water depths and the relatively high flow velo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::14c88dfb38ef58d2fa1f8c1b8afbe747
http://www.documentation.ird.fr/hor/fdi:010032492
http://www.documentation.ird.fr/hor/fdi:010032492
Autor:
Durand, Jean-René, Petit, Didier
The Java Sea is mainly a continental shelf with an average depht of 40 m and is controlled by the monsoon cycle : eastward current during North-West monsoon, westward current during South-East monsoon. Surface salinity is the best known parameter and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______932::045bf96aa9aefde2e1c75e6ee3bb82fa
http://www.documentation.ird.fr/hor/fdi:42768
http://www.documentation.ird.fr/hor/fdi:42768