TY  - THES
UR  - http://eprints.unpak.ac.id/4326/
PB  - Universitas Pakuan
AV  - none
M1  - Skripsi
A1  - Nur Sidik, Gema
A1  - Denih, Asep
A1  - Herdianto Situmorang, Boldson
TI  - ESTIMASI EVAPOTRANSPIRASI MENGGUNAKAN TEKNOLOGI 
PENGINDRAAN JAUH DI KOTA BOGOR
ID  - eprintsunpak4326
Y1  - 2021/08//
N2  - 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
ER  -