Geological survey professionnal paper, 917. A numerical model of material transport in salt-wedge estuaries / Fischer, H. B.

Public ISBD 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.

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