Condiciones de movimiento geostrofico para la corriente costera de Costa Rica (ING)

 

Zapisane w:
Opis bibliograficzny
Autor: Brenes, Carlos L.
Format: artículo original
Status:Versión publicada
Data wydania:1985
Opis:The geostrophic current and the volumen transport have been calculated, for the month of January 1969, for a section off Golfo Dulce, using the Montgomery´s method. During this period the Costa Rica Coastal Current was flowing northwestward, along the continental shelf, with a velocity up to 20cm/s, related to 67 cl/ton isanosteric surface. Under this current, a sub-surface flow in the opposite directions was found with an associated maximum velocity of 11 cm/s. The volume transport generated by these currents has been estimated  in about 1.26 Sv for the northwest current and 1.24 Sv for the southeast flow. In the first case, the total transport occurred at the surface layer, above the 250 cl/ ton isanoteric surface; in the second case, the transport shows up at in the layer between the 160 cl/ton and 200 cl/ton.At the southern end of the section, southeast and northwestward flows have been detected with velocities and transports of 33 cm/s, 0.55 Sv , and 39 cm/s, 3.54 Sv  respectively.
Kraj:Portal de Revistas UNA
Instytucja:Universidad Nacional de Costa Rica
Repositorio:Portal de Revistas UNA
Język:Español
OAI Identifier:oai:ojs.www.una.ac.cr:article/5347
Dostęp online:https://www.revistas.una.ac.cr/index.php/uniciencia/article/view/5347
Słowo kluczowe:Condiciones
geostrofico
corriente
costera