Search results for "BIOCLIMATOLOGIE"

showing 10 items of 10 documents

Penman-Monteith equation: How good is the "big leaf" ?

1996

International audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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Radiative surface temperature and convective flux calculation over crop canopies

1988

The analysis presented in this paper aims at a better understanding of the potential role of radiative temperature, as measured by a radiometer over crops, in sensible heat flux calculation. Defining radiative temperature as the mean temperature of the surfaces viewed by the radiometer (leaves and soil surface) and assuming that an Ohm's law type formula can be used to express sensible heat flux as a function of the difference between air temperature and radiative temperature, the aerodynamic resistance which divides this temperature difference has been analytically defined. The parameters which appear in the resistance expression depend essentially on wind velocity and canopy structure but…

Atmospheric ScienceCOUVERT VEGETAL010504 meteorology & atmospheric sciencesMeteorologyPlanetary boundary layer[SDV]Life Sciences [q-bio]Sensible heat01 natural sciencesPhysics::GeophysicsRadiative fluxRadiative transferMean radiant temperatureFLUX THERMIQUEPhysics::Atmospheric and Oceanic PhysicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesTEMPERATURE DE SURFACEPhysicsRadiometerBIOCLIMATOLOGIE04 agricultural and veterinary sciencesMechanicsMODELISATION[SDV] Life Sciences [q-bio]Heat fluxCONVECTIONHeat transfer040103 agronomy & agriculture0401 agriculture forestry and fisheries
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Executive summary, overview, conclusions and recommendations

1993

National audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUSTHERMOGRAPHIE IR
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Estimating the difference between brightness and surface temperatures for a vegetal canopy

1995

Abstract The difference between the surface temperature T S and the brightness temperature T b , which can be measured with a thermal infrared radiometer, has been calculated for different surface emissivity values and different atmospheric conditions. These calculations show that T s − T b is often significant even for high surface emissivities and that the spectral band in which the measurements are performed is a key factor in the interpretation of T s − T b . In particular, it is not a simple matter to use the characterisation of the whole spectrum atmospheric radiation to derive T s from T b when the measurements are performed in the 8–14 μm atmospheric window.

Surface (mathematics)Atmospheric ScienceBrightnessMaterials science010504 meteorology & atmospheric sciences0211 other engineering and technologiesAnalytical chemistry02 engineering and technology01 natural sciencesTemperature measurementOptics[SDV.SA.SF]Life Sciences [q-bio]/Agricultural sciences/Silviculture forestryEmissivityComputingMilieux_MISCELLANEOUS021101 geological & geomatics engineering0105 earth and related environmental sciencesGlobal and Planetary ChangeRadiometerBIOCLIMATOLOGIEbusiness.industryForestrySpectral bands13. Climate actionBrightness temperatureInfrared window[SDV.SA.SF] Life Sciences [q-bio]/Agricultural sciences/Silviculture forestrybusinessAgronomy and Crop ScienceAgricultural and Forest Meteorology
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An update for the definition of reference evapotranspiration

1994

International audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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An update for the calculation of reference evapotranspiration

1994

International audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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Evapotranspiration: Review of concepts and future trends

1996

International audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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Interactions surface continentale/atmosphère : l'expérience HAPEX-Sahel

1994

L'évolution saisonnière des termes du bilan radiatif, du bilan d'énergie et la production primaire d'une savane humide d'Afrique de l'Ouest (Lamto, Côte d'Ivoire) a été suivie dans le cadre du programme SAvanes à Long Terme (SALT). Ces données ont permis de développer un modèle de simulation des échanges surface/atmosphère en savane humide, basé sur les relations fonctionnelles existant entre la production et la phénologie de la savane d'une part, et les bilans d'énergie et hydrique de ce type de surface d'autre part. Ce modèle est issu du couplage de deux sous-modèles fonctionnant au pas de temps journalier et utilisant des variables climatiques standard en entrée : le modèle de bilan d'én…

BIOCLIMATOLOGIEEVAPOTRANSPIRATIONPRODUCTION PRIMAIRE[SDV]Life Sciences [q-bio]HYDROLOGIEBILAN HYDRIQUETRANSFERT RADIATIFSAVANEMODELISATION[SDV] Life Sciences [q-bio]BASSIN VERSANTPHENOLOGIERELATION SOL PLANTE ATMOSPHEREBILAN ENERGETIQUERECYCLAGE DE L'EAUComputingMilieux_MISCELLANEOUS
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Hypothèses et principes de la représentation de la diffusion du CO2 à différentes échelles, de la feuille au couvert

1995

National audience

[SDV] Life Sciences [q-bio][SDE] Environmental SciencesBIOCLIMATOLOGIE[SDV]Life Sciences [q-bio][SDE]Environmental SciencesComputingMilieux_MISCELLANEOUS
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Modelisation des echanges de masse et d'energie au niveau de couverts epars

1994

National audience

[SDV] Life Sciences [q-bio]BIOCLIMATOLOGIE[SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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