#TITLE_ALTERNATIVE#
Abstract: <br /> <br /> <br /> <br /> <br /> looding and dryness in a region watersheet happened as result of climate phenomenon, that is distribution rainfall to tend to happened during brief with high intensity, or drought period happened longer from his(its norm...
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| Format: | Theses |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/6275 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Abstract: <br />
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looding and dryness in a region watersheet happened as result of climate phenomenon, that is distribution rainfall to tend to happened during brief with high intensity, or drought period happened longer from his(its normal. In general flooding cause is input and system DAS. Input ( rain) covers rain factor of stress intensity, duration rainfall and distribution of rain, while system DAS covers topography factor, soil type, land use and system transfer of rain in DAS <br />
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Approximation of flooding debit which based on torrential rains can be classified in three ways that is, by the way of empiric formula, by the way of statistic or probability and by the way of unit hydrographer <br />
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