Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi

Mount Merapi is one of the active volcanos in Indonesia. This mount is located in Yogyakarta Special Province and Central Java Province. The Mount Merapi eruption can threat the thousands of people who live at around area of summit and the slope. The disaster risk happen when the eruption is happene...

全面介紹

Saved in:
書目詳細資料
Main Authors: , MUH THAHA, , Dr. Ir. Rachmad Jayadi, M.Eng.
格式: Theses and Dissertations NonPeerReviewed
出版: [Yogyakarta] : Universitas Gadjah Mada 2013
主題:
ETD
在線閱讀:https://repository.ugm.ac.id/125091/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=65256
標簽: 添加標簽
沒有標簽, 成為第一個標記此記錄!
機構: Universitas Gadjah Mada
id id-ugm-repo.125091
record_format dspace
spelling id-ugm-repo.1250912016-03-04T08:40:26Z https://repository.ugm.ac.id/125091/ Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi , MUH THAHA , Dr. Ir. Rachmad Jayadi, M.Eng. ETD Mount Merapi is one of the active volcanos in Indonesia. This mount is located in Yogyakarta Special Province and Central Java Province. The Mount Merapi eruption can threat the thousands of people who live at around area of summit and the slope. The disaster risk happen when the eruption is happened, but also there is lahar flood can be secondary disaster. Therefore, it is necessary to conduct a study to minimize the damage risk due to of this lahar flood. The study of extreme rainfall pattern that is happened at slope of Mount Merapi can be used to be information of lahar flood early warning system. The main material of this research is analyzing the extreme rainfall pattern by algebra averaging method at West and South slope of Mount Merapi. The analysis of extreme rainfall pattern spatially uses the rainfall data that was measured by automatic rainfall recorder. The analysis was done to select rainfall event with heterogeneous specific duration (unisolated event) for duration of 1, 2, 3 and 4 hours since years 1981-2007. Furthermore, interpolation was done to draw the rainfall spatial maps by Inverse Distance Method (IDW) using ArcGIS software. The results show the spatial pattern of extreme rainfall that is expressed in rainfall intensity variety to the duration. The most frequent extreme rainfall intensity happens in a specific area, at West and South West of Mount Merapi. The extreme rainfall events are found in rainfall recorder station of Ngandong, Ngepos, Girikerto, Gunung Maron and Argomulyo area. Moreover, the extreme rainfall events happen in month January, February, November and December. [Yogyakarta] : Universitas Gadjah Mada 2013 Thesis NonPeerReviewed , MUH THAHA and , Dr. Ir. Rachmad Jayadi, M.Eng. (2013) Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi. UNSPECIFIED thesis, UNSPECIFIED. http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=65256
institution Universitas Gadjah Mada
building UGM Library
country Indonesia
collection Repository Civitas UGM
topic ETD
spellingShingle ETD
, MUH THAHA
, Dr. Ir. Rachmad Jayadi, M.Eng.
Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
description Mount Merapi is one of the active volcanos in Indonesia. This mount is located in Yogyakarta Special Province and Central Java Province. The Mount Merapi eruption can threat the thousands of people who live at around area of summit and the slope. The disaster risk happen when the eruption is happened, but also there is lahar flood can be secondary disaster. Therefore, it is necessary to conduct a study to minimize the damage risk due to of this lahar flood. The study of extreme rainfall pattern that is happened at slope of Mount Merapi can be used to be information of lahar flood early warning system. The main material of this research is analyzing the extreme rainfall pattern by algebra averaging method at West and South slope of Mount Merapi. The analysis of extreme rainfall pattern spatially uses the rainfall data that was measured by automatic rainfall recorder. The analysis was done to select rainfall event with heterogeneous specific duration (unisolated event) for duration of 1, 2, 3 and 4 hours since years 1981-2007. Furthermore, interpolation was done to draw the rainfall spatial maps by Inverse Distance Method (IDW) using ArcGIS software. The results show the spatial pattern of extreme rainfall that is expressed in rainfall intensity variety to the duration. The most frequent extreme rainfall intensity happens in a specific area, at West and South West of Mount Merapi. The extreme rainfall events are found in rainfall recorder station of Ngandong, Ngepos, Girikerto, Gunung Maron and Argomulyo area. Moreover, the extreme rainfall events happen in month January, February, November and December.
format Theses and Dissertations
NonPeerReviewed
author , MUH THAHA
, Dr. Ir. Rachmad Jayadi, M.Eng.
author_facet , MUH THAHA
, Dr. Ir. Rachmad Jayadi, M.Eng.
author_sort , MUH THAHA
title Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
title_short Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
title_full Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
title_fullStr Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
title_full_unstemmed Analisi Pola Spasial Hujan Ekstrim Metode Rerata Aljabar di Wilayah Lereng Barat dan Selatan Gunung Merapi
title_sort analisi pola spasial hujan ekstrim metode rerata aljabar di wilayah lereng barat dan selatan gunung merapi
publisher [Yogyakarta] : Universitas Gadjah Mada
publishDate 2013
url https://repository.ugm.ac.id/125091/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=65256
_version_ 1681232200229453824