| Titre de série : |
U. S. Geological Survey Water Supply paper, 2280 |
| Titre : |
Magnitude and frequency of high flows of unregulated streams in Kansas |
| Type de document : |
texte imprimé |
| Auteurs : |
Jordan, P. R. |
| Mention d'édition : |
U.S. Geological Survey, Federal Center |
| Editeur : |
U.S. Geological Survey, Federal Center |
| Année de publication : |
1986 |
| ISBN/ISSN/EAN : |
CI-05043 |
| Note générale : |
Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... |
| Langues : |
Anglais (eng) |
| Mots-clés : |
Eau de surface Ruissellement Inondation Barrage Mesure et observation Prévention Sécurité des barrages |
| Index. décimale : |
627.8 Barrages |
| Résumé : |
Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... |
| Note de contenu : |
Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... |
U. S. Geological Survey Water Supply paper, 2280. Magnitude and frequency of high flows of unregulated streams in Kansas [texte imprimé] / Jordan, P. R. . - U.S. Geological Survey, Federal Center . - U.S. Geological Survey, Federal Center, 1986. ISSN : CI-05043 Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... Langues : Anglais ( eng)
| Mots-clés : |
Eau de surface Ruissellement Inondation Barrage Mesure et observation Prévention Sécurité des barrages |
| Index. décimale : |
627.8 Barrages |
| Résumé : |
Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... |
| Note de contenu : |
Information on high flow magnitude and frequency is needed for hydrologic evaluation of such factors as flood control storage and dam safety. High-flow magnitude and frequency data are given for 91 stream flow gaging stations throughout Kansas. Results of frequency calculations are given for durations of high flow of 1, 3, 7, 15, 15, 30, 60, 90, 120, and 183 consecutive days. Accuracy of the magnitude frequency values is influenced by the variability of flow, the number of years of flow record and the recurrence interval calculated... |
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