<> "The repository administrator has not yet configured an RDF license."^^ . <> . . . "ESTIMASI EVAPOTRANSPIRASI MENGGUNAKAN TEKNOLOGI \r\nPENGINDRAAN JAUH DI KOTA BOGOR"^^ . "iration carried out in Indonesia is carried out through \r\ndirect observation so that it only measures evapotranspiration at certain points. Remote \r\nsensing technology can be used to measure evapotranspiration widely because the data \r\nobtained is in the form of satellite images. This study focuses on the application of the ETindex \r\nEstimation Algorithm to calculate the value of the evapotranspiration index and the Penman�Monteith method to calculate the value of potential evapotranspiration, in which these two \r\nparameters are used to obtain the actual evapotranspiration value. In addition to satellite \r\nimagery, observational data from the Bogor Climatology Station is also used as supporting \r\nand comparison data. In areas with high vegetation, the range of values is 1.122 mm/day–\r\n1.326 mm/day, which is very different from the observed value, which is 3.9144 mm/day. \r\nAlthough the predicted value differs greatly from the observed value, the correlation between \r\nthe vegetation index, temperature, evapotranspiration index, and potential evapotranspiration \r\nindicates that the basis for this research and method is very much in line with previous studies.\r\nKeywords: evapotranspiration, remote sensing, satellite imagery, evapotranspiration indexiration carried out in Indonesia is carried out through \r\ndirect observation so that it only measures evapotranspiration at certain points. Remote \r\nsensing technology can be used to measure evapotranspiration widely because the data \r\nobtained is in the form of satellite images. This study focuses on the application of the ETindex \r\nEstimation Algorithm to calculate the value of the evapotranspiration index and the Penman�Monteith method to calculate the value of potential evapotranspiration, in which these two \r\nparameters are used to obtain the actual evapotranspiration value. In addition to satellite \r\nimagery, observational data from the Bogor Climatology Station is also used as supporting \r\nand comparison data. In areas with high vegetation, the range of values is 1.122 mm/day–\r\n1.326 mm/day, which is very different from the observed value, which is 3.9144 mm/day. \r\nAlthough the predicted value differs greatly from the observed value, the correlation between \r\nthe vegetation index, temperature, evapotranspiration index, and potential evapotranspiration \r\nindicates that the basis for this research and method is very much in line with previous studies.\r\nKeywords: evapotranspiration, remote sensing, satellite imagery, evapotranspiration index"^^ . "2021-08" . . "Universitas Pakuan"^^ . . . "Ilmu Komputer, Universitas Pakuan"^^ . . . . . . . . . . . . . . . . . "Boldson"^^ . "Herdianto Situmorang"^^ . "Boldson Herdianto Situmorang"^^ . . "Gema"^^ . "Nur Sidik"^^ . "Gema Nur Sidik"^^ . . "Asep"^^ . "Denih"^^ . "Asep Denih"^^ . . "Universitas Pakuan"^^ . . . "FMIPA"^^ . . . "lmu Komputer"^^ . . . . . . "HTML Summary of #4326 \n\nESTIMASI EVAPOTRANSPIRASI MENGGUNAKAN TEKNOLOGI \nPENGINDRAAN JAUH DI KOTA BOGOR\n\n" . "text/html" . . . "Ilmu Komputer"@en . .