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Titre de série : Agroclimatologie (CIEH) Titre : Etude régionale de l'évapotranspirtation potentielle : 1 - aspects méthodologiques et outils développés Type de document : texte imprimé Auteurs : Andé, N. ; Clauss, F. ; Minot, D. Mention d'édition : CIEH Editeur : CIEH Année de publication : 1989 ISBN/ISSN/EAN : CI-03280 Note générale : Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman. Langues : Français (fre) Mots-clés : Méthodologie Evaluation Evapotranspiration Evaporation Besoin en eau Pluviométrie Météorologie Formule de Penman Index. décimale : 551.57 Hydrométéorologie : brouillard, nuages, précipitations Résumé : Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman. Note de contenu : Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman. En ligne : etude_regionale_1989.pdf Agroclimatologie (CIEH). Etude régionale de l'évapotranspirtation potentielle : 1 - aspects méthodologiques et outils développés [texte imprimé] / Andé, N. ; Clauss, F. ; Minot, D. . - CIEH . - CIEH, 1989.
ISSN : CI-03280
Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman.
Langues : Français (fre)
Mots-clés : Méthodologie Evaluation Evapotranspiration Evaporation Besoin en eau Pluviométrie Météorologie Formule de Penman Index. décimale : 551.57 Hydrométéorologie : brouillard, nuages, précipitations Résumé : Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman. Note de contenu : Le présent rapport a pour but de présenter la méthodologie et les outils mis au point au CIEH pour la consitution d'une banque de données, l'analyse fréquentielle et spatiale de l'ETP évaluée par la formule de Penman. En ligne : etude_regionale_1989.pdf Réservation
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Titre : Etude des composantes du bilan d'énergie appliquée au calcul de l'évapotranspiration potentielle par différente formulation des formules de Penman et Penman-Montheith Type de document : texte imprimé Auteurs : Ag Mohamed Ali Ahmed Année de publication : 1992 ISBN/ISSN/EAN : ER 1541 Langues : Français (fre) Mots-clés : ENERGIE RAYONNEMENT SOLAIRE RADIATION ECHANGE THERMIQUE EVAPOTRANSPIRATION HYDROLOGIE CLIMATOLOGIE CHALEUR RAYONNEMENT THERMIQUE VENT FORMULE DE PENMAN FORMULE DE PENMAN-MONTHEITH Index. décimale : 531.6 Energie Etude des composantes du bilan d'énergie appliquée au calcul de l'évapotranspiration potentielle par différente formulation des formules de Penman et Penman-Montheith [texte imprimé] / Ag Mohamed Ali Ahmed . - 1992.
ISSN : ER 1541
Langues : Français (fre)
Mots-clés : ENERGIE RAYONNEMENT SOLAIRE RADIATION ECHANGE THERMIQUE EVAPOTRANSPIRATION HYDROLOGIE CLIMATOLOGIE CHALEUR RAYONNEMENT THERMIQUE VENT FORMULE DE PENMAN FORMULE DE PENMAN-MONTHEITH Index. décimale : 531.6 Energie Réservation
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Titre : The estimation of potential evapotranspiration using monograms to Penman's revised formula Type de document : texte imprimé Auteurs : Powell, F. A. Mention d'édition : Commonwealth of Australia Bureau of Meteorology Departement of the Interrior Editeur : Commonwealth of Australia Bureau of Meteorology Departement of the Interrior Année de publication : 1970 ISBN/ISSN/EAN : CI-05026 Note générale : The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates. Langues : Anglais (eng) Mots-clés : Evaporation Météorologie Climatologie Irrigation Hydrologie Hydraulique agricole Formule de Penman Index. décimale : 631.58 Méthodes de culture : jachère, assolement irrigation Résumé : The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates. Note de contenu : The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates. The estimation of potential evapotranspiration using monograms to Penman's revised formula [texte imprimé] / Powell, F. A. . - Commonwealth of Australia Bureau of Meteorology Departement of the Interrior . - Commonwealth of Australia Bureau of Meteorology Departement of the Interrior, 1970.
ISSN : CI-05026
The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates.
Langues : Anglais (eng)
Mots-clés : Evaporation Météorologie Climatologie Irrigation Hydrologie Hydraulique agricole Formule de Penman Index. décimale : 631.58 Méthodes de culture : jachère, assolement irrigation Résumé : The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates. Note de contenu : The use of modern watering techniques such as trickle irrigation enable the soil to be kept at field capacty. Under such conditions estimates of potential evapotranspiration should have a more pratical application. A nomogramm has been devised to provide a solution to the revised penman (1961) equation part of this nomogram can be employed to facilitate the preferential use of net, or global radiation also to include the ground heat flux term if this information is available. A wind function, for various values of the roughness parameter to, as devised by Businger (1956) has been incorporated in the aerodynamic component to the nomogramm. A facility is provided to allow for independent day-time and night-time variation of temperature, vapour pressure deficit, wind speed, atmospheric stability and roughness astimates. Réservation
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Titre : A method for the practical application of the Pennman formula for the estimation of potential evapotranspiration and evaporation from a free water surface Type de document : texte imprimé Auteurs : frère, M. Mention d'édition : FAO Editeur : FAO Année de publication : (s.d.) ISBN/ISSN/EAN : CI-04493 Note générale : The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration. Mots-clés : Evapotranspiration Evaporation Hydrologie Eau de surface Météorologie Formule de Penman Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration. Note de contenu : The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration. A method for the practical application of the Pennman formula for the estimation of potential evapotranspiration and evaporation from a free water surface [texte imprimé] / frère, M. . - FAO . - FAO, (s.d.).
ISSN : CI-04493
The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration.
Mots-clés : Evapotranspiration Evaporation Hydrologie Eau de surface Météorologie Formule de Penman Index. décimale : 551.3 Phénomènes de surface et exogènes et leurs agents : érosion Résumé : The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration. Note de contenu : The formula, designed in 1948 by Penman for the estimation of evaporation from a free water surface and of potentiel evapotranspiration from a vegetative cover, has been widely used throughout the world for the last 20 years with generally satisfactory results. Application of the formula in arid climates, as compared with field observations, seems to show an underestimation of the potentiel evapotranspiration. It must be kept in mind, however, that in these regions the energy balance is often disturbed by advection of hot dry air from the surroundings and a consequently harger evaporation from area, generally rather small, under consideration. Réservation
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