CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED

The increasedglobal climate directly affects theface of the earth. In addition to result in shifting of season and extremeweather, the relatively rapid change in temperaturebeing climate element also gives impact on intensity of geomorphology process (weathering, erosion, sedimentation). This paper...

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Main Author: Djoko Harmantyo
Format: Article
Language:English
Published: Universitas Gadjah Mada 2013-07-01
Series:Indonesian Journal of Geography
Online Access:https://jurnal.ugm.ac.id/ijg/article/view/2258
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spelling doaj-776599eb8e314a5baf627419e0faa0002020-11-25T02:03:37ZengUniversitas Gadjah MadaIndonesian Journal of Geography0024-95212354-91142013-07-0140210.22146/indo.j.geog,22582071CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHEDDjoko HarmantyoThe increasedglobal climate directly affects theface of the earth. In addition to result in shifting of season and extremeweather, the relatively rapid change in temperaturebeing climate element also gives impact on intensity of geomorphology process (weathering, erosion, sedimentation). This paper describes how the escalated climate affects the process 'of weathering and erosion as well as change in delta mainland size and its contribution to the emergence of spatial conflict. DAS Cimanukwas selected as the study case area. The escalated air temperature for a long period directly escalates the acceleration of rock weathering, which in turn accelerates the erosion of weathered rock due to rainfall to be sediment material through erosion process. During period of 1963 - 2002, Cimanuk delta area enlarged more than 350.000 m2/year. This new land, which is formed by weathering and erosion processes in the Cimanuk River Basin through peels of land surfacepredicted to be averagely more then 10 em/year. In the last, the new landformed by geomorphologic processes triggering the new source of conflict potentially.https://jurnal.ugm.ac.id/ijg/article/view/2258
collection DOAJ
language English
format Article
sources DOAJ
author Djoko Harmantyo
spellingShingle Djoko Harmantyo
CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
Indonesian Journal of Geography
author_facet Djoko Harmantyo
author_sort Djoko Harmantyo
title CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
title_short CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
title_full CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
title_fullStr CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
title_full_unstemmed CLIMATE S ROLE IN CHANGING THE FACE OF THE EARTH AND THE SPATIAL CONFLICT PROBLEMS: A PRELIMINARY STUDYON THE CIMANUK WATERSHED
title_sort climate s role in changing the face of the earth and the spatial conflict problems: a preliminary studyon the cimanuk watershed
publisher Universitas Gadjah Mada
series Indonesian Journal of Geography
issn 0024-9521
2354-9114
publishDate 2013-07-01
description The increasedglobal climate directly affects theface of the earth. In addition to result in shifting of season and extremeweather, the relatively rapid change in temperaturebeing climate element also gives impact on intensity of geomorphology process (weathering, erosion, sedimentation). This paper describes how the escalated climate affects the process 'of weathering and erosion as well as change in delta mainland size and its contribution to the emergence of spatial conflict. DAS Cimanukwas selected as the study case area. The escalated air temperature for a long period directly escalates the acceleration of rock weathering, which in turn accelerates the erosion of weathered rock due to rainfall to be sediment material through erosion process. During period of 1963 - 2002, Cimanuk delta area enlarged more than 350.000 m2/year. This new land, which is formed by weathering and erosion processes in the Cimanuk River Basin through peels of land surfacepredicted to be averagely more then 10 em/year. In the last, the new landformed by geomorphologic processes triggering the new source of conflict potentially.
url https://jurnal.ugm.ac.id/ijg/article/view/2258
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