Titre de série :	Geological survey professionnal paper, 917
Titre :	A numerical model of material transport in salt-wedge estuaries
Type de document :	texte imprimé
Auteurs :	Fischer, H. B. ; Stoner, D. J. ; Haushild, W. L.
Mention d'édition :	US Department of the Interior
Editeur :	US Department of the Interior
Année de publication :	1975
ISBN/ISSN/EAN :	CI-05512
Note générale :	Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.
Langues :	Anglais (eng)
Mots-clés :	Débit solide  Modèle mathématique  Informatisation  Salinité  Estuaire  Sédimentation
Index. décimale :	551 Géologie, météorologie, hydrologie générale
Résumé :	Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.
Note de contenu :	Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.

Geological survey professionnal paper, 917. A numerical model of material transport in salt-wedge estuaries [texte imprimé] / Fischer, H. B. ; Stoner, D. J. ; Haushild, W. L.  . -  US Department of the Interior . - US Department of the Interior, 1975.
ISSN : CI-05512
Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.
Langues : Anglais (eng)

Mots-clés :	Débit solide  Modèle mathématique  Informatisation  Salinité  Estuaire  Sédimentation
Index. décimale :	551 Géologie, météorologie, hydrologie générale
Résumé :	Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.
Note de contenu :	Water in a salt-wedge estuary ideally is characterized by an oscillating well-mixed wedge of undiluted seawater topped by a series of successively more dilute overlying layers. In the wedge the flow is entrained upward into the overlying layer. The report describes required input data and method of operation of the computer program.