12 research outputs found

    Value of distributed water level and soil moisture data in the evaluation of a distributed hydrological model: Application to the PUMMA model in the Mercier catchment (6.6 km2) in France

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    This paper emphasizes the importance of integrating outlet discharge and observed internal variables in the evaluation of distributed hydrological models outputs. It proposes a general methodology for a diagnostic evaluation of a complex distributed hydrological model, based on discharge data at the outlet and additional distributed information such as water level and surface soil moisture data. The proposed methodology is illustrated using the PUMMA model in the Mercier sub-catchment (6.6 km2). Model parameters are specified according to field data and a previous study performed in a neighbouring catchment (Jankowfsky et al., 2014), without calibration. The distributed water level and soil moisture network of sensors were useful in the model evaluation process. Thus, model parameters are specified either using in situ information or results from previous studies. A stepwise approach is used for model evaluation. It includes standard water balance assessment as well as comparison of observed and simulated outlet discharge, whether on annual or event timescales. Soil moisture sensors are used to assess the ability of the model to simulate seasonal water storage dynamics based on a normalized index. The water level sensors network is used on two timescales: on a seasonal timescale, sensors network is used to assess the model’s ability to simulate intermittency; whereas on event timescales, sensors network is used in determining the model’s ability to reproduce observed reaction as well as response times. Event timescales do also focus on the correlation between hydrological response and either rainfall event or antecedent soil moisture variables. Results show that the non-calibrated model is quite effective at capturing water flow and soil water-storage dynamics, but it fails to reproduce observed runoff volume during events. There is strong indication of a deficiency in the characterization of catchment storage and upstream flowpath description. The soil water content and a network of water level sensors provide interesting information about soil moisture and river flow dynamics. They however fail to provide quantitative information about catchment storage. This study opens interesting perspectives for the evaluation of distributed hydrological models using hydrological signatures. Furthermore, it highlights the requirement of quantitative as well as qualitative signatures for improving such models

    Sistema E-Business para vinedos J.Bouchon

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    106 p.El objetivo principal de este proyecto es realizar un plan de inserción de los viñedos J. Bouchon en los negocios ON-LINE (negocios a través de Internet) del sistema E-Business, de tal manera de buscar en el corto plazo un mecanismo de comercialización que le permita a la empresa acceder a los mercados de destinos mas exclusivos. La idea central es solucionar el problema de rigidez en los canales de distribución internacionales que se presentan en la actualidad. Creemos indispensable dar los pasos de incorporación de este tipo de negocios en la empresa, para hacerlas mas competitivas, con la incorporación de las ventajas que presenta este sistema (reducción de costos de operación, expedita gestión tanto con proveedores como con los clientes, no existencia de tributos al traspaso de información), al generar un alto grado de flexibilidad en el proceso de comercialización de sus productos a través del sistema E - Business

    The 16th Data Release of the Sloan Digital Sky Surveys: First Release from the APOGEE-2 Southern Survey and Full Release of eBOSS Spectra

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    This paper documents the 16th data release (DR16) from the Sloan Digital Sky Surveys (SDSS), the fourth and penultimate from the fourth phase (SDSS-IV). This is the first release of data from the Southern Hemisphere survey of the Apache Point Observatory Galactic Evolution Experiment 2 (APOGEE-2); new data from APOGEE-2 North are also included. DR16 is also notable as the final data release for the main cosmological program of the Extended Baryon Oscillation Spectroscopic Survey (eBOSS), and all raw and reduced spectra from that project are released here. DR16 also includes all the data from the Time Domain Spectroscopic Survey and new data from the SPectroscopic IDentification of ERosita Survey programs, both of which were co-observed on eBOSS plates. DR16 has no new data from the Mapping Nearby Galaxies at Apache Point Observatory (MaNGA) survey (or the MaNGA Stellar Library "MaStar"). We also preview future SDSS-V operations (due to start in 2020), and summarize plans for the final SDSS-IV data release (DR17)

    The 16th Data Release of the Sloan Digital Sky Surveys : First Release from the APOGEE-2 Southern Survey and Full Release of eBOSS Spectra

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    This paper documents the 16th data release (DR16) from the Sloan Digital Sky Surveys (SDSS), the fourth and penultimate from the fourth phase (SDSS-IV). This is the first release of data from the Southern Hemisphere survey of the Apache Point Observatory Galactic Evolution Experiment 2 (APOGEE-2); new data from APOGEE-2 North are also included. DR16 is also notable as the final data release for the main cosmological program of the Extended Baryon Oscillation Spectroscopic Survey (eBOSS), and all raw and reduced spectra from that project are released here. DR16 also includes all the data from the Time Domain Spectroscopic Survey and new data from the SPectroscopic IDentification of ERosita Survey programs, both of which were co-observed on eBOSS plates. DR16 has no new data from the Mapping Nearby Galaxies at Apache Point Observatory (MaNGA) survey (or the MaNGA Stellar Library "MaStar"). We also preview future SDSS-V operations (due to start in 2020), and summarize plans for the final SDSS-IV data release (DR17).Peer reviewe

    The Fifteenth Data Release of the Sloan Digital Sky Surveys: First Release of MaNGA-derived Quantities, Data Visualization Tools, and Stellar Library

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    Twenty years have passed since first light for the Sloan Digital Sky Survey (SDSS). Here, we release data taken by the fourth phase of SDSS (SDSS-IV) across its first three years of operation (2014 July–2017 July). This is the third data release for SDSS-IV, and the 15th from SDSS (Data Release Fifteen; DR15). New data come from MaNGA—we release 4824 data cubes, as well as the first stellar spectra in the MaNGA Stellar Library (MaStar), the first set of survey-supported analysis products (e.g., stellar and gas kinematics, emission-line and other maps) from the MaNGA Data Analysis Pipeline, and a new data visualization and access tool we call "Marvin." The next data release, DR16, will include new data from both APOGEE-2 and eBOSS; those surveys release no new data here, but we document updates and corrections to their data processing pipelines. The release is cumulative; it also includes the most recent reductions and calibrations of all data taken by SDSS since first light. In this paper, we describe the location and format of the data and tools and cite technical references describing how it was obtained and processed. The SDSS website (www.sdss.org) has also been updated, providing links to data downloads, tutorials, and examples of data use. Although SDSS-IV will continue to collect astronomical data until 2020, and will be followed by SDSS-V (2020–2025), we end this paper by describing plans to ensure the sustainability of the SDSS data archive for many years beyond the collection of data

    The fifteenth data release of the Sloan Digital Sky Surveys : first release of MaNGA derived quantities, data visualization tools and stellar library

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    Twenty years have passed since first light for the Sloan Digital SkySurvey (SDSS). Here, we release data taken by the fourth phase of SDSS(SDSS-IV) across its first three years of operation (July 2014-July2017). This is the third data release for SDSS-IV, and the fifteenth from SDSS (Data Release Fifteen; DR15). New data come from MaNGA - we release 4824 datacubes, as well as the first stellar spectra in the MaNGA Stellar Library (MaStar), the first set of survey-supported analysis products (e.g. stellar and gas kinematics, emission line, andother maps) from the MaNGA Data Analysis Pipeline (DAP), and a new data visualisation and access tool we call "Marvin". The next data release, DR16, will include new data from both APOGEE-2 and eBOSS; those surveys release no new data here, but we document updates and corrections to their data processing pipelines. The release is cumulative; it also includes the most recent reductions and calibrations of all data taken by SDSS since first light. In this paper we describe the location and format of the data and tools and cite technical references describing how it was obtained and processed. The SDSS website (www.sdss.org) has also been updated, providing links to data downloads, tutorials and examples of data use. While SDSS-IV will continue to collect astronomical data until 2020, and will be followed by SDSS-V(2020-2025), we end this paper by describing plans to ensure the sustainability of the SDSS data archive for many years beyond the collection of data.Publisher PDFPeer reviewe

    Automatización del Procesamiento de Unidades de Respuesta Hidrológica (URHs) con GRASS para un Modelo Hidrológico Distribuido

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    El uso de modelos hidrológicos distribuidos en cuencas periurbanas requiere definir en forma efectiva la unidad espacial que se utiliza para el análisis. Entre los distintos tipos de discretización se encuentran las Unidades de Respuesta Hidrológica (URHs), que permiten representar en forma explícita diferentes elementos, tales como, áreas impermeables, canales artificiales, colectores de aguas lluvias y calles que pueden modificar significativamente la dirección del flujo superficial. En este estudio se abordan los requerimientos del modelo hidrológico PUMMA (PeriUrban Model for landscape Management), donde ciertos parámetros como la distancia entre centros de gravedad de las URHs, ubicación de la red de flujo, y la longitud del perímetro influyen directamente en la extracción de la red de flujo superficial, sub-superficial y los niveles de agua subterráneos. En la malla de entrada se corrigieron aquellos elementos mal-formados, que corresponden a polígonos de forma irregular, con bordes mal representados y con el centro de gravedad fuera del polígono. Para identificar estos elementos se utilizaron descriptores de forma, resultando el Índice de Convexidad como el mejor descriptor, con un valor límite de 0.75. Se abordaron problemas como ajuste de contornos y suavización de bordes con ángulos rectos, también se realizó un proceso de segmentación espacial que consideró criterios como distribución homogénea de pendiente, convexidad y tamaño máximo de las URHs, en el que se aplicó un enfoque de triangulación y disolución mediante criterio de convexidad limite. Todas estas tareas fueron implementadas mediante el uso del software GRASS-GIS y rutinas escritas en Python. El pre-procesamiento automático se aplicó en dos cuencas peri-urbanas francesas, Mercier y Chaudanne, con 7.3 km2 y 4.1 km2 respectivamente. Se considera sustancial el mejoramiento obtenido en la red de drenaje de ambas mallas optimizadas, en la que se obtuvo una representación más realista de las líneas de flujo, tanto en longitud como en trayectoria
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