#TITLE_ALTERNATIVE#
<p align="justify">Increasing the value of extreme discharge was influenced by changes in land cover with fixed rainfall assumption. But changes in extreme rainfall over the last few decades have had an effect on extreme discharge as well. By calculating the extreme rainfall ratios a...
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id-itb.:293262018-06-06T13:53:43Z#TITLE_ALTERNATIVE# Rifqi Fathin Fawwaz Muzaeni (12813002) , Muhammad Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/29326 <p align="justify">Increasing the value of extreme discharge was influenced by changes in land cover with fixed rainfall assumption. But changes in extreme rainfall over the last few decades have had an effect on extreme discharge as well. By calculating the extreme rainfall ratios and extreme discharges obtained by taking 5% of the daily data in two different periods, the magnitude of each parameter changes. The ratio was obtained from the comparison between the return period value. The results show an extreme rainfall ratio of 1.16 times can affect extreme discharge changes in Ciliwung Watershed. Meanwhile, the frequency and maximum value of extreme rainfall at CH>00s were more and greater than CH<00s. This indicates that the dominant maximum frequency change and maximum rainfall values affect extreme discharge changes in the Ciliwung Watershed.<p align="justify"> text |
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<p align="justify">Increasing the value of extreme discharge was influenced by changes in land cover with fixed rainfall assumption. But changes in extreme rainfall over the last few decades have had an effect on extreme discharge as well. By calculating the extreme rainfall ratios and extreme discharges obtained by taking 5% of the daily data in two different periods, the magnitude of each parameter changes. The ratio was obtained from the comparison between the return period value. The results show an extreme rainfall ratio of 1.16 times can affect extreme discharge changes in Ciliwung Watershed. Meanwhile, the frequency and maximum value of extreme rainfall at CH>00s were more and greater than CH<00s. This indicates that the dominant maximum frequency change and maximum rainfall values affect extreme discharge changes in the Ciliwung Watershed.<p align="justify"> |
| format |
Final Project |
| author |
Rifqi Fathin Fawwaz Muzaeni (12813002) , Muhammad |
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Rifqi Fathin Fawwaz Muzaeni (12813002) , Muhammad #TITLE_ALTERNATIVE# |
| author_facet |
Rifqi Fathin Fawwaz Muzaeni (12813002) , Muhammad |
| author_sort |
Rifqi Fathin Fawwaz Muzaeni (12813002) , Muhammad |
| title |
#TITLE_ALTERNATIVE# |
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#TITLE_ALTERNATIVE# |
| title_full |
#TITLE_ALTERNATIVE# |
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#TITLE_ALTERNATIVE# |
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#TITLE_ALTERNATIVE# |
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https://digilib.itb.ac.id/gdl/view/29326 |
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