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Tehnical report TR, 137. Régional maximun flood peaks in Southern Africa / Kovacs, Z.
Titre de série : Tehnical report TR, 137 Titre : Régional maximun flood peaks in Southern Africa Type de document : texte imprimé Auteurs : Kovacs, Z. Mention d'édition : DWA Editeur : DWA Année de publication : 1988 ISBN/ISSN/EAN : CI-03730 Note générale : The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods. Langues : Anglais (eng) Mots-clés : Hydrologie Inondation Pluviométrie Classification Comparaison Calcul Captage de l'eau Catalogue Index. décimale : 551.48 Hydrologie : Résumé : The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods. Note de contenu : The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods. Tehnical report TR, 137. Régional maximun flood peaks in Southern Africa [texte imprimé] / Kovacs, Z. . - DWA . - DWA, 1988.
ISSN : CI-03730
The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods.
Langues : Anglais (eng)
Mots-clés : Hydrologie Inondation Pluviométrie Classification Comparaison Calcul Captage de l'eau Catalogue Index. décimale : 551.48 Hydrologie : Résumé : The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods. Note de contenu : The regional maximum flood (FMF) in an empirirically established upper limit of flood peaks that can be reasonably expected at a given site. The proposed method for the estimation of RMF is a revised and updated version of departemental technical report TR 105 published in 1980 the method is based on maximum flood speaks recorded since 19856 at more than 500 sites in Southern Africa. The relative flood peak magnitude is expressed by the Francou-roudier regional coefficient K. Eight maximum observed 3 days rainfall and catchement caracteristics. The perspective K enveloppe were established by taking onto account the number of and quality of data. The RMF can be instanly calculated in the geographic position of the site and its catchment areas are konow. Owing its consistency the RMF campares favourably with results obtained by other methods. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B730.61256 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61255 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61254 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61253 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61252 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61251 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61250 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B730.61249 CI-03730 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible