Principal component analysis for identifying period of seasons in Indonesia

The seasonal variability of Indonesian rainfall is almost entirely controlled by the Asian monsoon and so displays two distinct seasons, i.e. wet and dry seasons with transition periods in between. The onset of the monsoon varies with places, therefore, when dealing with seasonal rainfall, different...

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Main Author: Dewi Galuh Condro Kirono
Format: Article
Language:English
Published: Universitas Gadjah Mada 2013-07-01
Series:Indonesian Journal of Geography
Subjects:
Online Access:https://jurnal.ugm.ac.id/ijg/article/view/2211
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spelling doaj-c61b51ecf6a140cc8f88ada4e54425312020-11-25T02:56:05ZengUniversitas Gadjah MadaIndonesian Journal of Geography0024-95212354-91142013-07-0136210.22146/indo.j.geog,22112026Principal component analysis for identifying period of seasons in IndonesiaDewi Galuh Condro KironoThe seasonal variability of Indonesian rainfall is almost entirely controlled by the Asian monsoon and so displays two distinct seasons, i.e. wet and dry seasons with transition periods in between. The onset of the monsoon varies with places, therefore, when dealing with seasonal rainfall, different researchers/authors have different way referring to the seasons. Hence, one definition may not be appropriate for all places. This problem creates a necessity for identifying the period of the season so that it can be used for Indonesia as a whole. This paper examines the spatial variation of the seasons over the Indonesia region and demonstrates the application of Principal Component Analysis (PCA) to solve the above mentioned problem, namely to identify the period of the seasons in Indonesia as a unity. The analysis is performed using monthly rainfall data from 63 stations spread across the country covering the period of 1947 to 1999 (52 years). The results support the fact that the wet season onset starts early in the northwestern part of Sumatra and propagates eastward and southward. It is not surprising if the north-western part of the country experiences a longer wet season than the east-northern part does. It is also shown that PCA is a useful tool for identifying the period of the season in Indonesia. Through the analysis, it is found that there are three types of rainfalls which have important influence on the year to year variation of the annual rainfall, i.e: the wet season (December to March), the dry season (May to September), and the dry-to-wet transition (October to November).https://jurnal.ugm.ac.id/ijg/article/view/2211Principal Component Analysis, Season period, Indonesia.
collection DOAJ
language English
format Article
sources DOAJ
author Dewi Galuh Condro Kirono
spellingShingle Dewi Galuh Condro Kirono
Principal component analysis for identifying period of seasons in Indonesia
Indonesian Journal of Geography
Principal Component Analysis, Season period, Indonesia.
author_facet Dewi Galuh Condro Kirono
author_sort Dewi Galuh Condro Kirono
title Principal component analysis for identifying period of seasons in Indonesia
title_short Principal component analysis for identifying period of seasons in Indonesia
title_full Principal component analysis for identifying period of seasons in Indonesia
title_fullStr Principal component analysis for identifying period of seasons in Indonesia
title_full_unstemmed Principal component analysis for identifying period of seasons in Indonesia
title_sort principal component analysis for identifying period of seasons in indonesia
publisher Universitas Gadjah Mada
series Indonesian Journal of Geography
issn 0024-9521
2354-9114
publishDate 2013-07-01
description The seasonal variability of Indonesian rainfall is almost entirely controlled by the Asian monsoon and so displays two distinct seasons, i.e. wet and dry seasons with transition periods in between. The onset of the monsoon varies with places, therefore, when dealing with seasonal rainfall, different researchers/authors have different way referring to the seasons. Hence, one definition may not be appropriate for all places. This problem creates a necessity for identifying the period of the season so that it can be used for Indonesia as a whole. This paper examines the spatial variation of the seasons over the Indonesia region and demonstrates the application of Principal Component Analysis (PCA) to solve the above mentioned problem, namely to identify the period of the seasons in Indonesia as a unity. The analysis is performed using monthly rainfall data from 63 stations spread across the country covering the period of 1947 to 1999 (52 years). The results support the fact that the wet season onset starts early in the northwestern part of Sumatra and propagates eastward and southward. It is not surprising if the north-western part of the country experiences a longer wet season than the east-northern part does. It is also shown that PCA is a useful tool for identifying the period of the season in Indonesia. Through the analysis, it is found that there are three types of rainfalls which have important influence on the year to year variation of the annual rainfall, i.e: the wet season (December to March), the dry season (May to September), and the dry-to-wet transition (October to November).
topic Principal Component Analysis, Season period, Indonesia.
url https://jurnal.ugm.ac.id/ijg/article/view/2211
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