Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City

Karangmumus RBA to getting degradation pressure being concrete drying and flooding so much to frighten. Climate data from BMG Temindung and SPAS Lempake has to water balance analysis based on Hewlett and Nutter methode. This region have the Area Class III (1500–2000 mm/year). With the bimodel or dou...

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Main Author: Ismail
Format: Article
Language:English
Published: Universitas Indonesia 2009-11-01
Series:Makara Seri Sains
Subjects:
Online Access:http://journal.ui.ac.id/science/article/view/416
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author Ismail
author_facet Ismail
author_sort Ismail
collection DOAJ
description Karangmumus RBA to getting degradation pressure being concrete drying and flooding so much to frighten. Climate data from BMG Temindung and SPAS Lempake has to water balance analysis based on Hewlett and Nutter methode. This region have the Area Class III (1500–2000 mm/year). With the bimodel or double wave rainfall models with C patern. The hight rainfall depth periode at December and April, therefore the low rainfall depth at September and November. Have level Q = ± 9.9%, or rainfall tipe A (very wet area with tropical wet vegetation) and E1 agroclimte zone. Water balance monthly indicated that this area have to water surplus 8 month, i.e. January (27.0 mm), February (57.3 mm), March (119.7 mm), April (72.8 mm), May (48.4 mm), Juni (19.6 mm), November (58.7 mm) and December (75.3 mm), or total amounts water surplus 478.8 mm/year. The water deficits at Juni (0.4 mm), July (0.3 mm), Augus (3.9 mm), September (13.6 mm) and October (26.7 mm) or total amount water deficits (44.5 mm/year).
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spelling doaj.art-b200c91ca761463fad27b68962279ff22022-12-21T22:02:23ZengUniversitas IndonesiaMakara Seri Sains1693-66712009-11-01132151156Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda CityIsmailKarangmumus RBA to getting degradation pressure being concrete drying and flooding so much to frighten. Climate data from BMG Temindung and SPAS Lempake has to water balance analysis based on Hewlett and Nutter methode. This region have the Area Class III (1500–2000 mm/year). With the bimodel or double wave rainfall models with C patern. The hight rainfall depth periode at December and April, therefore the low rainfall depth at September and November. Have level Q = ± 9.9%, or rainfall tipe A (very wet area with tropical wet vegetation) and E1 agroclimte zone. Water balance monthly indicated that this area have to water surplus 8 month, i.e. January (27.0 mm), February (57.3 mm), March (119.7 mm), April (72.8 mm), May (48.4 mm), Juni (19.6 mm), November (58.7 mm) and December (75.3 mm), or total amounts water surplus 478.8 mm/year. The water deficits at Juni (0.4 mm), July (0.3 mm), Augus (3.9 mm), September (13.6 mm) and October (26.7 mm) or total amount water deficits (44.5 mm/year).journal.ui.ac.id/science/article/view/416water balancedKarangmumus river basin area (RBA)
spellingShingle Ismail
Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
Makara Seri Sains
water balanced
Karangmumus river basin area (RBA)
title Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
title_full Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
title_fullStr Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
title_full_unstemmed Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
title_short Water Balance Analysis at Karangmumus River Basin Area (RBA) Samarinda City
title_sort water balance analysis at karangmumus river basin area rba samarinda city
topic water balanced
Karangmumus river basin area (RBA)
url http://journal.ui.ac.id/science/article/view/416
work_keys_str_mv AT ismail waterbalanceanalysisatkarangmumusriverbasinarearbasamarindacity