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Estimation of regional evapotranspiration by TM/ETM+ data over heterogeneous surfaces / S. Liu in Photogrammetric Engineering & Remote Sensing, PERS, vol 73 n° 10 (October 2007)
[article]
Titre : Estimation of regional evapotranspiration by TM/ETM+ data over heterogeneous surfaces Type de document : Article/Communication Auteurs : S. Liu, Auteur ; G. Hu, Auteur ; et al., Auteur Année de publication : 2007 Article en page(s) : pp 1169 - 1178 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] analyse diachronique
[Termes IGN] bilan hydrique
[Termes IGN] données météorologiques
[Termes IGN] estimation quantitative
[Termes IGN] évapotranspiration
[Termes IGN] image Landsat-ETM+
[Termes IGN] image Landsat-TM
[Termes IGN] Pékin (Chine)
[Termes IGN] surface hétérogèneRésumé : (Auteur) Evapotranspiration is an important part in surface energy balance and water balance. Compared with other methods (micrometeorological, climatological, or hydrological method), the remote sensing model has obvious superiority to estimate regional evapotranspiration over heterogeneous surfaces. In this study, based on Landsat TM/ETM+ data and meteorological data, evapotranspiration in Beijing area on 17 April 2001, 12 April 2002, 06 July 2004, 06 May 2005, and 22 May 2005 were calculated by an estimation model of regional evapotranspiration. Comparisons of energy balance components (net radiation, soil heat flux, sensible and latent heat flux) with measured fluxes were made integrating the remotely sensed fluxes by the footprint model. Results show that latent heat flux estimates (adjusted for closure) with errors (MBE1RMSE) 26.47142.54 Wm-2, sensible heat flux error of -8.56123.79 Wm-2, net radiation error of 25.16150.87 Wm-2 and soil heat flux error of 10.68122.81 Wm-2. The better agreement between the estimates and the measurements indicates that the remote sensing model is appropriate for estimating regional evapotranspiration over heterogeneous surfaces. Furthermore, the spatial distribution of evapotranspiration in Beijing area was analyzed. Copyright ASPRS Numéro de notice : A2007-477 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article DOI : 10.14358/PERS.73.10.1169 En ligne : https://doi.org/10.14358/PERS.73.10.1169 Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28840
in Photogrammetric Engineering & Remote Sensing, PERS > vol 73 n° 10 (October 2007) . - pp 1169 - 1178[article]Estimating spatial patterns of rainfall interception from remotely sensed vegetation indices and spectral mixture analysis / S.M. de Jong in International journal of geographical information science IJGIS, vol 21 n° 5 (may 2007)
[article]
Titre : Estimating spatial patterns of rainfall interception from remotely sensed vegetation indices and spectral mixture analysis Type de document : Article/Communication Auteurs : S.M. de Jong, Auteur ; V.G. Jetten, Auteur Année de publication : 2007 Article en page(s) : pp 529 - 545 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] analyse des mélanges spectraux
[Termes IGN] érosion hydrique
[Termes IGN] évapotranspiration
[Termes IGN] image HYMAP
[Termes IGN] image hyperspectrale
[Termes IGN] indice de végétation
[Termes IGN] Leaf Area Index
[Termes IGN] pluie
[Termes IGN] ruissellementRésumé : (Auteur) Rainfall interception by vegetation is an important factor in the water balance. Consequently, rainfall interception should also be an important factor in models simulating processes such as evaporation, transpiration, surface runoff, soil erosion, and crop growth. In practice, however, it is difficult to make quantitative assessments of the spatial and temporal distribution of rainfall interception loss at the catchment level, for instance, and to make these values available as model input. In this paper, we present a novel method using earth observation images to estimate local quantitative values of rainfall interception loss. Leaf Area Index (LAI) and fractional vegetation cover per grid cell are important process variables for rainfall interception. These two variables are estimated from images using spectral vegetation indices and using spectral mixture analysis, respectively. Relations between canopy storage capacity and LAI exist for several plant species and vegetation types, but limited data are found on crops, and more research is needed in this field. The new method is explained and illustrated for a study area in southern France with a variety of land-cover types. It is found to be a valuable and practical approach to quantitatively assess spatial patterns of interception loss for given rainfall events. Copyright Taylor & Francis Numéro de notice : A2007-135 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article DOI : 10.1080/13658810601064884 En ligne : https://doi.org/10.1080/13658810601064884 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28498
in International journal of geographical information science IJGIS > vol 21 n° 5 (may 2007) . - pp 529 - 545[article]Exemplaires(2)
Code-barres Cote Support Localisation Section Disponibilité 079-07031 RAB Revue Centre de documentation En réserve L003 Disponible 079-07032 RAB Revue Centre de documentation En réserve L003 Disponible Integration of MODIS data into a simple model for the spatial distributed simulation of soil water content and evapotranspiration / Y. Zhang in Remote sensing of environment, vol 104 n° 4 (30/10/2006)
[article]
Titre : Integration of MODIS data into a simple model for the spatial distributed simulation of soil water content and evapotranspiration Type de document : Article/Communication Auteurs : Y. Zhang, Auteur ; M. Wegehenkel, Auteur Année de publication : 2006 Article en page(s) : pp 393 - 408 Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Applications de télédétection
[Termes IGN] Allemagne
[Termes IGN] analyse diachronique
[Termes IGN] évapotranspiration
[Termes IGN] humidité du sol
[Termes IGN] image Terra-MODIS
[Termes IGN] Leaf Area Index
[Termes IGN] réflectance
[Termes IGN] simulationRésumé : (Auteur) A precise simulation of soil water content (SWC) and actual evapotranspiration (ETa) in a region or a catchment depends on the accuracy of the spatial data inputs. In this study, we developed a simple grid-based soil water balance model. In this model, remotely sensed vegetation data are used to estimate spatial distributions of daily SWC and ETa rates. The model was validated by comparing simulated SWC with the measured by gravimetric method and time domain reflectometry (TDR) at an experimental test site located in Northeastern Germany in the time period 1993–1998. The index of agreement IA and the root-mean-square error obtained from the comparison of the TDR measurements to the simulated values ranged from 0.45 to 0.80 and from 0.029 to 0.061 cm3/cm3, respectively. The comparison of simulated ETa rates to those measured by four large-scale lysimeters at another test site showed IA values above 0.87 and R2 values higher than 0.59. For the regional application of the model, a method was developed to integrate the Moderate Resolution Imaging Spectrometer (MODIS) vegetation data into the model. The MODIS data used in our study consist of 16-day normalized difference vegetation index and 8-day leaf area index products. Regarding the spatial application of the model, our approach was tested in a catchment located in Northeastern Germany in 2001–2003. A sufficient correlation between daily discharge rates measured at two observation gauges in the catchment and the corresponding simulated discharge rates and also good correlations between the simulated ETa rates and the MODIS-leaf area index values indicate that the model is an appropriate simulation tool at regional scale if the corresponding additional spatial databases regarding surface and soil properties are available. Copyright Elsevier Numéro de notice : A2006-496 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1016/j.rse.2006.05.011 En ligne : https://doi.org/10.1016/j.rse.2006.05.011 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=28220
in Remote sensing of environment > vol 104 n° 4 (30/10/2006) . - pp 393 - 408[article]Heat and drought 2003 in Europe: a climate synthesis / Martine Rebetez in Annals of Forest Science, Vol 63 n° 6 (september 2006)
[article]
Titre : Heat and drought 2003 in Europe: a climate synthesis Titre original : La chaleur et la sécheresse 2003 : une synthèse climatique Type de document : Article/Communication Auteurs : Martine Rebetez, Auteur ; Helmut Mayer, Auteur ; Olivier Dupont, Auteur ; Dirk Schindler, Auteur ; Karl Gartner, Auteur ; Jürgen P. Kropp, Auteur ; Anette Menzel, Auteur Année de publication : 2006 Article en page(s) : pp. 569 - 577 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Termes IGN] évapotranspiration
[Termes IGN] précipitation
[Termes IGN] sécheresse
[Termes IGN] surveillance météorologique
[Termes IGN] température
[Vedettes matières IGN] Végétation et changement climatiqueRésumé : (auteur) Heat and drought were extreme in summer 2003 in Europe. Climatic data show that most extreme were maximum air temperatures in June and August; maps of these two months show a striking similarity in geographical range. Over wide regions, monthly mean temperatures were more than 4 °C above the long term mean values. The heat lasted from May to September in large parts of western and central Europe. The lack of precipitation was most severe in summer 2003 but precipitation was generally below normal from February 2003 until June 2004 (with the exception of two months). Sunshine duration was above normal, particularly in regions which usually have rainy and cloudy episodes in summer, and relative air humidity was below normal during the whole year of 2003. The drought experienced by the vegetation in summer 2003 was exacerbated by the length of the period with scarce precipitation and humidity, by the heat during the summer and by long sunshine duration. Numéro de notice : A2006-666 Affiliation des auteurs : non IGN Thématique : FORET Nature : Article DOI : 10.1051/forest:2006043 Date de publication en ligne : 14/09/2006 En ligne : https://doi.org/10.1051/forest:2006043 Format de la ressource électronique : url article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=72706
in Annals of Forest Science > Vol 63 n° 6 (september 2006) . - pp. 569 - 577[article]Exemplaires(1)
Code-barres Cote Support Localisation Section Disponibilité IFN-001-P000644 PER Revue Nogent-sur-Vernisson Archives périodiques Exclu du prêt Canopy directional emissivity: comparison between models / J.A. Sobrino in Remote sensing of environment, vol 99 n° 3 (30/11/2005)
[article]
Titre : Canopy directional emissivity: comparison between models Type de document : Article/Communication Auteurs : J.A. Sobrino, Auteur ; J.C. Jimenez-Munoz, Auteur ; W. Verhoef, Auteur Année de publication : 2005 Article en page(s) : pp 304 - 314 Note générale : Bibliographie Langues : Anglais (eng) Descripteur : [Vedettes matières IGN] Traitement d'image
[Termes IGN] analyse comparative
[Termes IGN] couvert végétal
[Termes IGN] emissivité
[Termes IGN] évapotranspiration
[Termes IGN] modèle de transfert radiatif
[Termes IGN] radiance
[Termes IGN] rayonnement infrarouge thermique
[Termes IGN] température au solRésumé : (Auteur) Land surface temperature plays an important role in many environmental studies, as for example the estimation of heat fluxes and evapotranspiration. In order to obtain accurate values of land surface temperature, atmospheric, emissivity and angular effects should be corrected. This paper focuses on the analysis of the angular variation of canopy emissivity, which is an important variable that has to be known to correct surface radiances and obtain surface temperatures. Emissivity is also involved in the atmospheric corrections since it appears in the reflected, downwelling atmospheric term. For this purpose, five different methods for simulating directional canopy emissivity have been analyzed and compared. The five methods are composed of two geometrical models, developed by Sobrino et al. and Snyder and Wan, in which the vegetation is considered as an opaque medium, and three are based on radiative transfer models, developed by François et al., Snyder and Wan and Verhoef et al., in which the vegetation is considered as a turbid medium. Over surfaces with sparse and low vegetation cover, high angular variations of canopy emissivity are obtained, with differences between at-nadir view and 80° of 0.03. Over fully vegetated surfaces angular effects on emissivity are negligible when radiative transfer models are applied, so in these situations the angular variations on emissivity are not critical on the retrieved land surface temperature from remote sensing data. Angular variations on emissivity are lower when the emissivity of the soil and the emissivity of the vegetation are closer. All the models considered assume Lambertian behaviour for the soil and the leaves. This assumption is also discussed, showing a different behaviour of directional canopy emissivity when a non-Lambertian soil is considered. Numéro de notice : A2005-459 Affiliation des auteurs : non IGN Thématique : IMAGERIE Nature : Article nature-HAL : ArtAvecCL-RevueIntern DOI : 10.1016/j.rse.2005.09.005 En ligne : https://doi.org/10.1016/j.rse.2005.09.005 Format de la ressource électronique : URL article Permalink : https://documentation.ensg.eu/index.php?lvl=notice_display&id=27595
in Remote sensing of environment > vol 99 n° 3 (30/11/2005) . - pp 304 - 314[article]Predicting riparian evapotranspiration from MODIS vegetation indices and meteorological data / P. Nagler in Remote sensing of environment, vol 94 n° 1 (15/01/2005)PermalinkCombining weather prediction and remote sensing data for the calculation of evapotranspiration rates: application to Denmark / E. Boegh in International Journal of Remote Sensing IJRS, vol 25 n° 13 (July 2004)PermalinkEvaporing estimation in the Yellow River basin, China using integrated NDVI data / R. Sun in International Journal of Remote Sensing IJRS, vol 25 n° 13 (July 2004)PermalinkPermalinkUtilisation des données SPOT pour la cartographie d'un bilan de l'eau simplifié / M.J. Lefevre-Fonollosa in Bulletin du comité français de cartographie, n° 142 - 143 (mars - août 1995)PermalinkUne approche uniformisée du calcul de l'évapotranspiration potentielle pour l'ensemble des pays de la communauté européenne / E. Choisnel (1992)PermalinkPrésentation d'un modèle de transfert couplé de masse et de chaleur dans le système sol-végétation-atmosphère pour les zones arides et semi-arides / Abdelghani Chehbouni (1992)PermalinkUtilisation des données satellitaires dans les modèles météorologiques / H.P. Randriamanantena (1992)PermalinkEstimation of tropical forest canopy temperatures, thermal response numbers, and evapotranspiration using an aircraft-based thermal sensor / J.C. Luvall in Photogrammetric Engineering & Remote Sensing, PERS, vol 56 n° 10 (october 1990)PermalinkGeocoding and stereo display of tropical forest multisensor datasets / R. Welch in Photogrammetric Engineering & Remote Sensing, PERS, vol 56 n° 10 (october 1990)Permalink