@InProceedings{CurtarelliRennAlcā:2012:EfCoFr,
               author = "Curtarelli, Marcelo Pedroso and Renn{\'o}, Camilo Daleles and 
                         Alc{\^a}ntara, Enner Herenio de",
          affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Effects of cold front passage and atmospheric boundary layer 
                         stability in the estimates of spatially distributed heat fluxes in 
                         a tropical reservoir",
            booktitle = "Anais...",
                 year = "2012",
                pages = "5246--5249",
         organization = "IEEE International Geoscience and Remote Sensing Symposium, 32. 
                         (IGARSS).",
            publisher = "IEEE",
             keywords = "Heat transfer , MODIS , Reservoirs , Stability criteria , Thermal 
                         stability , Water heating, Sensoriamento remoto, Limnologia 
                         f{\'{\i}}sica, Fluxos de calor, Reservat{\'o}rios.",
             abstract = "Sensible and latent heat fluxes were estimated over a large 
                         tropical hydroelectric reservoir under cold front conditions. In 
                         situ and satellite data were used to adjust the bulk coefficients 
                         for momentum and heat exchanges between water and atmosphere and 
                         spatialize the sensible and latent heat fluxes over the reservoir. 
                         The results showed that during a cold front event the sensible and 
                         latent heat fluxes can be up to three times greater than the 
                         fluxes before and after the cold front passage. The main source of 
                         heat loss to atmosphere during the cold front passage was the 
                         evaporation (i.e. latent heat) reaching values near to 500 W m-2. 
                         The highest values of heat loss were observed at littoral zone and 
                         some embayment of reservoir. The increase in wind speed and 
                         decrease in air temperature and humidity during the cold front 
                         event were the main factors that influenced the heat loss.",
  conference-location = "Munich",
      conference-year = "22-27 July 2012",
                  doi = "10.1109/IGARSS.2012.6352426",
                  url = "http://dx.doi.org/10.1109/IGARSS.2012.6352426",
                 isbn = "978-1-4673-1158-8 and 978-1-4673-1160-1",
                 issn = "2153-6996",
                label = "lattes: 7417849872779783 1 CurtarelliRennAlc{\^a}:2012:EfCoFr",
             language = "en",
           targetfile = "06352426.pdf",
        urlaccessdate = "30 abr. 2024"
}