@Article{ZaninSaty:2021:NuMoCo,
               author = "Zanin, Paulo R. and Satyamurty, Prakki",
          affiliation = "{Instituto Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Numerical modeling of coseismic tropospheric disturbances arising 
                         from the unstable acoustic gravity wave energetics",
              journal = "Journal of Hydrometeorology",
                 year = "2021",
               volume = "22",
               number = "6",
                pages = "1609--1625",
                month = "June",
             keywords = "Evapotranspiration, Hydrologic cycle, Precipitation, Soil 
                         moisture, South America, Water vapor.",
             abstract = "The interseasonal and interbasins hydrological coupling between 
                         the Amazon and the La Plata watersheds is obtained with the help 
                         of ERA-5 atmospheric reanalysis, MERGE/CPTEC precipitation, GLEAM 
                         evapotranspiration, and the GLDAS/Noah soil moisture datasets. The 
                         hypotheses formulated in a previous work by Zanin and Satyamurty 
                         about the hydrological processes interconnecting the Amazon Basin 
                         and the La Plata Basin are tested. A new method for finding the 
                         sourcesink relationships among the boxes (regions) is presented. 
                         The precipitation recycling, frequency of sourcesink behaviors, 
                         the soil moisture memory, and the continental moisture transport 
                         between remote regions are evaluated. The main result of this 
                         study is that the amount of water precipitated over the 
                         southeastern region of the Amazon Basin at the end of the South 
                         American monsoon during the autumn season influences the amount of 
                         precipitation during the winter season over the central-western 
                         region of the La Plata Basin.",
                  doi = "10.1175/JHM-D-20-0080.1",
                  url = "http://dx.doi.org/10.1175/JHM-D-20-0080.1",
                 issn = "1525-755X",
             language = "en",
        urlaccessdate = "09 maio 2024"
}