Hydrological pattern of Pahang River basin and their relation to flood historical event

Pahang River is the main channel to drain off water from the inundated area of Pahang Basin to the South China Sea during wet season which is caused by the northeast monsoon. Most of the inundations of lower areas of Pahang River Basin were caused by overflowing of the Pahang River. The statistics o...

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Main Authors:	Pan, Ia Lun, Muhd. Barzani Gasim, Mohd. Ekhwan Toriman, Sahibin Abd. Rahim, Khairul Amri Kamaruddin
Format:	Article
Language:	English
Published:	Journal of Faculty of Social Sciences and Humanities. Universiti Kebangsaan Malaysia 2011
Online Access:	http://journalarticle.ukm.my/2664/ http://journalarticle.ukm.my/2664/ http://journalarticle.ukm.my/2664/1/alan011.pdf

id	ukm-2664
recordtype	eprints
spelling	ukm-26642016-12-14T06:32:16Z http://journalarticle.ukm.my/2664/ Hydrological pattern of Pahang River basin and their relation to flood historical event Pan, Ia Lun Muhd. Barzani Gasim, Mohd. Ekhwan Toriman, Sahibin Abd. Rahim, Khairul Amri Kamaruddin, Pahang River is the main channel to drain off water from the inundated area of Pahang Basin to the South China Sea during wet season which is caused by the northeast monsoon. Most of the inundations of lower areas of Pahang River Basin were caused by overflowing of the Pahang River. The statistics of rainfall and hydrological factors were calculated in terms of their means for the period from 1980 to 2009. The highest water level recorded at Sg. Yap was 45.36m and the lowest was 43.49m, whereas for Temerloh, the highest water level was 26.71m and the lowest was 24.73m. Lubuk Paku had the highest water level of 15.23m and the lowest was recorded as 12.70m. Besides that, the highest monthly total rainfall at Sg.Yap was 254.01mm and the lowest was 106.67mm. At Temerloh, the highest monthly total rainfall was 219.83mm and the lowest was 93.75mm. At Lubuk Paku, the highest monthly total rainfall was 324.57mm and the lowest was 79.81mm. The mean discharge of Pahang River (1980-2009) at Sg. Yap was 845.78m³/s, at Temerloh was 1008.50m³/s and Lubuk Paku was 1184.46m³/s. The water levels which beyond the danger level in recent three decades had also been identified. Journal of Faculty of Social Sciences and Humanities. Universiti Kebangsaan Malaysia 2011 Article PeerReviewed application/pdf en http://journalarticle.ukm.my/2664/1/alan011.pdf Pan, Ia Lun and Muhd. Barzani Gasim, and Mohd. Ekhwan Toriman, and Sahibin Abd. Rahim, and Khairul Amri Kamaruddin, (2011) Hydrological pattern of Pahang River basin and their relation to flood historical event. e-BANGI: Jurnal Sains Sosial dan Kemanusiaan, 6 (1). pp. 29-37. ISSN 1823-884x http://www.ukm.my/e-bangi
repository_type	Digital Repository
institution_category	Local University
institution	Universiti Kebangasaan Malaysia
building	UKM Institutional Repository
collection	Online Access
language	English
description	Pahang River is the main channel to drain off water from the inundated area of Pahang Basin to the South China Sea during wet season which is caused by the northeast monsoon. Most of the inundations of lower areas of Pahang River Basin were caused by overflowing of the Pahang River. The statistics of rainfall and hydrological factors were calculated in terms of their means for the period from 1980 to 2009. The highest water level recorded at Sg. Yap was 45.36m and the lowest was 43.49m, whereas for Temerloh, the highest water level was 26.71m and the lowest was 24.73m. Lubuk Paku had the highest water level of 15.23m and the lowest was recorded as 12.70m. Besides that, the highest monthly total rainfall at Sg.Yap was 254.01mm and the lowest was 106.67mm. At Temerloh, the highest monthly total rainfall was 219.83mm and the lowest was 93.75mm. At Lubuk Paku, the highest monthly total rainfall was 324.57mm and the lowest was 79.81mm. The mean discharge of Pahang River (1980-2009) at Sg. Yap was 845.78m³/s, at Temerloh was 1008.50m³/s and Lubuk Paku was 1184.46m³/s. The water levels which beyond the danger level in recent three decades had also been identified.
format	Article
author	Pan, Ia Lun Muhd. Barzani Gasim, Mohd. Ekhwan Toriman, Sahibin Abd. Rahim, Khairul Amri Kamaruddin,
spellingShingle	Pan, Ia Lun Muhd. Barzani Gasim, Mohd. Ekhwan Toriman, Sahibin Abd. Rahim, Khairul Amri Kamaruddin, Hydrological pattern of Pahang River basin and their relation to flood historical event
author_facet	Pan, Ia Lun Muhd. Barzani Gasim, Mohd. Ekhwan Toriman, Sahibin Abd. Rahim, Khairul Amri Kamaruddin,
author_sort	Pan, Ia Lun
title	Hydrological pattern of Pahang River basin and their relation to flood historical event
title_short	Hydrological pattern of Pahang River basin and their relation to flood historical event
title_full	Hydrological pattern of Pahang River basin and their relation to flood historical event
title_fullStr	Hydrological pattern of Pahang River basin and their relation to flood historical event
title_full_unstemmed	Hydrological pattern of Pahang River basin and their relation to flood historical event
title_sort	hydrological pattern of pahang river basin and their relation to flood historical event
publisher	Journal of Faculty of Social Sciences and Humanities. Universiti Kebangsaan Malaysia
publishDate	2011
url	http://journalarticle.ukm.my/2664/ http://journalarticle.ukm.my/2664/ http://journalarticle.ukm.my/2664/1/alan011.pdf
first_indexed	2023-09-18T19:36:42Z
last_indexed	2023-09-18T19:36:42Z
_version_	1777405318643318784

Hydrological pattern of Pahang River basin and their relation to flood historical event

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