Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia

Global Climate change has been discussed in the High-Level Conference in Rio de Janeiro, Brazil in 1992 and has given more impacts in the world. One of the global climate exchanges is the rising of intensity and frequency of climate extreme which included drought, flood, and hurricane. The objective...

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Main Authors: Sutapa I Wayan, Galib Ishak Muhammad, Wim Andiese Vera
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:MATEC Web of Conferences
Online Access:https://www.matec-conferences.org/articles/matecconf/pdf/2019/25/matecconf_icancee2019_04003.pdf
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spelling doaj-04717edc662c48bc849902ce28812d3a2021-04-02T14:51:09ZengEDP SciencesMATEC Web of Conferences2261-236X2019-01-012760400310.1051/matecconf/201927604003matecconf_icancee2019_04003Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, IndonesiaSutapa I Wayan0Galib Ishak Muhammad1Wim Andiese Vera2Department of Civil Engineering, Universitas TadulakoDepartment of Civil Engineering, Universitas TadulakoDepartment of Civil Engineering, Universitas TadulakoGlobal Climate change has been discussed in the High-Level Conference in Rio de Janeiro, Brazil in 1992 and has given more impacts in the world. One of the global climate exchanges is the rising of intensity and frequency of climate extreme which included drought, flood, and hurricane. The objective of this study was to investigate the effects of climate change on evapotranspiration and rainfall for river water discharge of Rawa. The investigation has been carried out using daily data and analyzed on a daily, monthly and yearly. The rain stations that represent the location of this research are Palolo, Kulawi, and Wuasa. Climatological station nearest to the research station used Bora. Climate trends and projected changes in the method of Makesens analysis (Mann-Kendall, Sens) and the correlation of rainfall and evapotranspiration discharge used linear regression equation. Similarly, the correlation between changes in soil water storage with rainfall, evapotranspiration, and discharge was analyzed in a linear manner. The conclusion of this study is the climate changes in the River of Rawa watershed was characterized by slowly increasing temperature, increasing rainfall, and decreasing discharge.https://www.matec-conferences.org/articles/matecconf/pdf/2019/25/matecconf_icancee2019_04003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Sutapa I Wayan
Galib Ishak Muhammad
Wim Andiese Vera
spellingShingle Sutapa I Wayan
Galib Ishak Muhammad
Wim Andiese Vera
Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
MATEC Web of Conferences
author_facet Sutapa I Wayan
Galib Ishak Muhammad
Wim Andiese Vera
author_sort Sutapa I Wayan
title Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
title_short Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
title_full Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
title_fullStr Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
title_full_unstemmed Impact of climate change on rawa river water source in lake Lindu watershed, Central Sulawesi, Indonesia
title_sort impact of climate change on rawa river water source in lake lindu watershed, central sulawesi, indonesia
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2019-01-01
description Global Climate change has been discussed in the High-Level Conference in Rio de Janeiro, Brazil in 1992 and has given more impacts in the world. One of the global climate exchanges is the rising of intensity and frequency of climate extreme which included drought, flood, and hurricane. The objective of this study was to investigate the effects of climate change on evapotranspiration and rainfall for river water discharge of Rawa. The investigation has been carried out using daily data and analyzed on a daily, monthly and yearly. The rain stations that represent the location of this research are Palolo, Kulawi, and Wuasa. Climatological station nearest to the research station used Bora. Climate trends and projected changes in the method of Makesens analysis (Mann-Kendall, Sens) and the correlation of rainfall and evapotranspiration discharge used linear regression equation. Similarly, the correlation between changes in soil water storage with rainfall, evapotranspiration, and discharge was analyzed in a linear manner. The conclusion of this study is the climate changes in the River of Rawa watershed was characterized by slowly increasing temperature, increasing rainfall, and decreasing discharge.
url https://www.matec-conferences.org/articles/matecconf/pdf/2019/25/matecconf_icancee2019_04003.pdf
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