An Investigation of Variation in Vegetation Canopy with Hemispherical Photography and Satellite Data

P. [1-9] [9]

• Capitoli dello stesso volume (disponibili singolarmente)

  • Preface ; Acknowledgments
    Ottieni capitolo
  • Development of a Web Based Model to Process and Analyse Remotely Sensed Data Sets
    Ottieni capitolo
  • Mesoscale Study of the Climatic Parameters in the Eastern Region of Paraguay
    Ottieni capitolo
  • Estimation of Forest Canopy Gap Fraction Changes Through the Application of Terrestrial Laser Scanner and Hemispherical Photo Camera
    Ottieni capitolo
  • Impacts of Climate Change on Soil Erosion within a Specific Area Investigated by the Ciomta Project
    Ottieni capitolo
  • A Preliminary Evaluation of the Cropsyst Model for Sugarcane in the Southeast of Brazil
    Ottieni capitolo
  • Estimation of Soil Moisture for the Valencia Anchor Station Region (VAS) by Using Temperature-Vegetation Dryness Index (TVDI) Obtained from Modis Satellite Images
    Ottieni capitolo
  • Co2 Measurement and Data Processing in Order to Assess the Effect of Climate Change on Natural Ecosystems
    Ottieni capitolo
  • Increasing the Quality of Data Sets for Studies of Climate Change in South America
    Ottieni capitolo
  • The Study of Climate Change on the Hydrology of the Itaipu Hydropower Basin
    Ottieni capitolo
  • Precipitation and Temperature Trend Evaluation in Paraguay Using Brams Model
    Ottieni capitolo
  • Exploring Land Use in the Litoral Argentino, by Remote Sensing Techniques Applied to the Classification of Sac C Satelite Imagery
    Ottieni capitolo
  • Determination and Analysis of the Standardized Precipitation Index (spi) as Drought Intensity Indicator for Paraguay
    Ottieni capitolo
  • An Investigation of Variation in Vegetation Canopy with Hemispherical Photography and Satellite Data
  • Characterizing Drought Events in Cuiabá, Mt, Brazil, with Standard Precipitation (SPI)
    Ottieni capitolo

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  Codice DOI: 10.1400/116367

  Permalink: http://digital.casalini.it/10.1400/116367