ESTIMASI EVAPOTRANSPIRASI MENGGUNAKAN TEKNOLOGI PENGINDRAAN JAUH DI KOTA BOGOR

Nur Sidik, Gema and Denih, Asep and Herdianto Situmorang, Boldson (2021) ESTIMASI EVAPOTRANSPIRASI MENGGUNAKAN TEKNOLOGI PENGINDRAAN JAUH DI KOTA BOGOR. Skripsi thesis, Universitas Pakuan.

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Abstract

iration carried out in Indonesia is carried out through direct observation so that it only measures evapotranspiration at certain points. Remote sensing technology can be used to measure evapotranspiration widely because the data obtained is in the form of satellite images. This study focuses on the application of the ETindex Estimation 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 parameters are used to obtain the actual evapotranspiration value. In addition to satellite imagery, observational data from the Bogor Climatology Station is also used as supporting and comparison data. In areas with high vegetation, the range of values is 1.122 mm/day– 1.326 mm/day, which is very different from the observed value, which is 3.9144 mm/day. Although the predicted value differs greatly from the observed value, the correlation between the vegetation index, temperature, evapotranspiration index, and potential evapotranspiration indicates that the basis for this research and method is very much in line with previous studies. Keywords: evapotranspiration, remote sensing, satellite imagery, evapotranspiration indexiration carried out in Indonesia is carried out through direct observation so that it only measures evapotranspiration at certain points. Remote sensing technology can be used to measure evapotranspiration widely because the data obtained is in the form of satellite images. This study focuses on the application of the ETindex Estimation 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 parameters are used to obtain the actual evapotranspiration value. In addition to satellite imagery, observational data from the Bogor Climatology Station is also used as supporting and comparison data. In areas with high vegetation, the range of values is 1.122 mm/day– 1.326 mm/day, which is very different from the observed value, which is 3.9144 mm/day. Although the predicted value differs greatly from the observed value, the correlation between the vegetation index, temperature, evapotranspiration index, and potential evapotranspiration indicates that the basis for this research and method is very much in line with previous studies. Keywords: evapotranspiration, remote sensing, satellite imagery, evapotranspiration index

Item Type: Thesis (Skripsi)
Subjects: Fakultas Ilmu Pengetahuan Alam dan Matematika > Ilmu Komputer
Divisions: Fakultas Matematika dan Ilmu Pengetahuan Alam > Ilmu Komputer
Depositing User: PERPUSTAKAAN FAKULTAS MATEMATIKA DAN ILMU PENGETAHUAN ALAM UNPAK
Date Deposited: 03 Sep 2022 03:32
Last Modified: 03 Sep 2022 17:11
URI: http://eprints.unpak.ac.id/id/eprint/4326

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