Persistence in surface overflow of Andean rivers

The temporal structure of both deficit (negative) and excess (positive) periods in surface overflow of Andean rivers were analyzed by studying the runs. In Southern areas (in the province of Neuquén and the Southern part of the province of Mendoza), positive and negative groups of anomalies have bee...

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Guardado en:
Detalles Bibliográficos
Autores principales: Minetti, Juan L., Carletto, Martha C.
Formato: Articulo
Lenguaje:Inglés
Publicado: 1994
Materias:
Geofísica
surface overflow
escurrimiento superficial
Neuquén
San Juan
Mendoza
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/135371
Aporte de:
SEDICI (UNLP) de Universidad Nacional de La Plata

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