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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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 |
work_keys_str_mv |
AT sutapaiwayan impactofclimatechangeonrawariverwatersourceinlakelinduwatershedcentralsulawesiindonesia AT galibishakmuhammad impactofclimatechangeonrawariverwatersourceinlakelinduwatershedcentralsulawesiindonesia AT wimandiesevera impactofclimatechangeonrawariverwatersourceinlakelinduwatershedcentralsulawesiindonesia |
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