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Journal of hydrology. Review of field observations of runoff generation in the tropics / Dubreuil, P. L.
Titre de série : Journal of hydrology Titre : Review of field observations of runoff generation in the tropics Type de document : texte imprimé Auteurs : Dubreuil, P. L. Année de publication : April 1985 ISBN/ISSN/EAN : CI-05038 Note générale : Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow. Langues : Anglais (eng) Mots-clés : Hydrologie Eau de surface Ruissellement Climat Index. décimale : 551.48 Hydrologie : Résumé : Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow. Note de contenu : Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow. Journal of hydrology. Review of field observations of runoff generation in the tropics [texte imprimé] / Dubreuil, P. L. . - April 1985.
ISSN : CI-05038
Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow.
Langues : Anglais (eng)
Mots-clés : Hydrologie Eau de surface Ruissellement Climat Index. décimale : 551.48 Hydrologie : Résumé : Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow. Note de contenu : Over the last thirty years, french hydrologists have observed flow characteristics at the outlets 7 small tropical watersheds, characteristics which vary between arid zones, humid zones and equatorial rainforest zones. The main physical phenomena related to be various types of runoff generation have been observed and analysed. The generation of runoff subsurface, runof following tropical rainstorms depends on oil surface formation, texture and structure as well as vegetation cover, geological substrats, we athered material and climat. Analysis is also made of exprimental rainfall - runoff relationships, the shape of flood hydrographs and the conditions necessary for the occurence of steady hase flow. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B038.199186 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199185 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199184 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199183 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199182 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199181 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199180 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B038.199179 CI-05038 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible Journal of hydrology, 102. Hydrological persistance characteristics of floods and drought - Interregional comparisons / Takeuchi, K.
Titre de série : Journal of hydrology, 102 Titre : Hydrological persistance characteristics of floods and drought - Interregional comparisons Type de document : texte imprimé Auteurs : Takeuchi, K. Année de publication : 1988 ISBN/ISSN/EAN : CI-08021 Note générale : Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world... Langues : Anglais (eng) Mots-clés : Hydrologie Inondation Sécheresse Ruissellement Climatologie Géographie PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world... Note de contenu : Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world... Journal of hydrology, 102. Hydrological persistance characteristics of floods and drought - Interregional comparisons [texte imprimé] / Takeuchi, K. . - 1988.
ISSN : CI-08021
Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world...
Langues : Anglais (eng)
Mots-clés : Hydrologie Inondation Sécheresse Ruissellement Climatologie Géographie PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world... Note de contenu : Flood and drought duration curves (FDC and DDC) are defined and some sample curve of precipitation and stream flow series are plotted on logarithmic papers. FDC an DDC represent persistence characteristics of hydrological time series when they assume high and low values respectively. They contain information that has direct implications on water resources management both for flood control and for water use. Daily and monthly precipitation and streamflow data were collected at six stations in Japan and twelve stations in various parts of the world... Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B021.62744 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62743 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62742 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62741 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62740 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62739 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62738 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B021.62737 CI-08021 Monographie Bibliothèque CDI-Ouaga Fond documentaire Disponible Journal of hydrology. Effects of spatial variability and scale with implication to hydrologic modeling / Wood, E. F.
Titre de série : Journal of hydrology Titre : Effects of spatial variability and scale with implication to hydrologic modeling Type de document : texte imprimé Auteurs : Wood, E. F. ; Sivapalan, M. ; Beven, R. Année de publication : 1988 ISBN/ISSN/EAN : CI-08017 Note générale : This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull... Langues : Anglais (eng) Mots-clés : Hydrologie Sol Topographie PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull... Note de contenu : This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull... Journal of hydrology. Effects of spatial variability and scale with implication to hydrologic modeling [texte imprimé] / Wood, E. F. ; Sivapalan, M. ; Beven, R. . - 1988.
ISSN : CI-08017
This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull...
Langues : Anglais (eng)
Mots-clés : Hydrologie Sol Topographie PRECIPITATIONS Index. décimale : 551.48 Hydrologie : Résumé : This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull... Note de contenu : This paper reports the results of a preliminary investigation into the existence of representative elementary area (REA) in the content of hydrologic modeling at the catchment scale. The investigation was carried out for an actual catchment topography as represented by Cowecta river experimentation basin with synthetic realizations for rainfall and soils. The hydrologic response of this catchment was modeled by a modified version of top model, which is capable of modeling both infiltration excess and saturation excess runoff and incorporating the spatial variability of soils topography, and rainfull... Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B017.62729 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62730 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62731 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62732 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62733 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62734 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62735 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B017.62736 CI-08017 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible Journal of hydrology. Towards a delimitation of southwestern Nigeria into hydrological regions / Ogunkoya, O. O.
Titre de série : Journal of hydrology Titre : Towards a delimitation of southwestern Nigeria into hydrological regions Type de document : texte imprimé Auteurs : Ogunkoya, O. O. Mention d'édition : Elsevier science publishers B.V Editeur : Elsevier science publishers B.V Année de publication : 1988 ISBN/ISSN/EAN : CI-02086 Note générale : Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern. Langues : Anglais (eng) Mots-clés : Hydrologie Drainage Géologie Bassin versant Index. décimale : 551.48 Hydrologie : Résumé : Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern. Note de contenu : Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern. Journal of hydrology. Towards a delimitation of southwestern Nigeria into hydrological regions [texte imprimé] / Ogunkoya, O. O. . - Elsevier science publishers B.V . - Elsevier science publishers B.V, 1988.
ISSN : CI-02086
Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern.
Langues : Anglais (eng)
Mots-clés : Hydrologie Drainage Géologie Bassin versant Index. décimale : 551.48 Hydrologie : Résumé : Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern. Note de contenu : Hydrological regionalization in southwester Nigeria appears to be influenced by drainage basin geology while percentage area of the basin underlain by massive quartzites could be used as an index of occurence of desirable hydrologic response pattern. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI03B086.62273 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62274 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62275 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62276 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62277 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62278 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62279 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI03B086.62280 CI-02086 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible Journal of hydrology. Evapotranspiration estimates derived from subsoil salinity data / Mathias, A. D.
Titre de série : Journal of hydrology Titre : Evapotranspiration estimates derived from subsoil salinity data Type de document : texte imprimé Auteurs : Mathias, A. D. ; Hassan, H. M. ; Yu-qi Hu Année de publication : 1986 ISBN/ISSN/EAN : CI-11683 Note générale : A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution. Langues : Anglais (eng) Mots-clés : Evapotranspiration Irrigation Salinité Eau souterraine Evaporation precipitations Méthodologie Sol Index. décimale : 631.58 Méthodes de culture : jachère, assolement irrigation Résumé : A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution. Note de contenu : A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution. Journal of hydrology. Evapotranspiration estimates derived from subsoil salinity data [texte imprimé] / Mathias, A. D. ; Hassan, H. M. ; Yu-qi Hu . - 1986.
ISSN : CI-11683
A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution.
Langues : Anglais (eng)
Mots-clés : Evapotranspiration Irrigation Salinité Eau souterraine Evaporation precipitations Méthodologie Sol Index. décimale : 631.58 Méthodes de culture : jachère, assolement irrigation Résumé : A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution. Note de contenu : A method is described for estimating past evapotranspiration (ET) rates from irrigated fields. Its is based on the assumption that salt concentrations below the crop root zone are a function f the flux of naturally occuring salt applied by irrigation at the soil surface and the rate of soil water depletion due to Et. Thus, if irrigation histories and subsoil salinity are available, ET rates may be calculed. For irrigation field with low leaching fractions, corrections to the ET estimates by may be necessary due to chemical precipitation. This is done through modeling of chemistry of from the use of observed chloride concentrations in solution. Réservation
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Code-barres Cote Support Localisation Section Disponibilité CI04B683.73681 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73682 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73683 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73684 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73685 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73686 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73687 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible CI04B683.73688 CI-11683 Périodique Bibliothèque CDI-Ouaga Fond documentaire Disponible Journal of hydrology. Observation rainfall-runoff analysis for estimating effects of cloud seeding on water resources in northern Israel / Benjamini, Y.
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