Peran Data Indeks Monsun Global Dan Iod Terhadap Perilaku Curah Hujan Di Beberapa Kawasan Indonesia
Main Author: | Eddy Hermawan |
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Format: | Book |
Bahasa: | ind |
Terbitan: |
LAPAN
, 2011
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Subjects: | |
Online Access: |
http://repository.lapan.go.id//index.php?p=show_detail&id=3979 http://repository.lapan.go.id//lib/phpthumb/phpThumb.php?src=../../images/docs/SNSAA2011.PNG.PNG |
ctrlnum |
slims-3979 |
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fullrecord |
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<dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title>Peran Data Indeks Monsun Global Dan Iod Terhadap Perilaku Curah Hujan Di Beberapa Kawasan Indonesia</title><creator>Eddy Hermawan</creator><subject>Dipole Mode</subject><subject>Monsoon</subject><subject>Rainfall</subject><publisher>LAPAN</publisher><date>2011</date><language>ind</language><type>Book:Book</type><identifier>http://repository.lapan.go.id//index.php?p=show_detail&id=3979</identifier><identifier>978-979-1458-53-5</identifier><description>Interactions that occurred between the Monsoon and IOD (Indian Ocean Dipole) are still kept under review, especially its impact on rainfall anomalies that occurred in several regions of Indonesia. Based on the results of the analysis of global Monsoon index of each parameter is represented by ISMI (Indian Summer Monsoon Index), WNPMI (Western North Pacific Monsoon Index), and AUSMI (Australian Monsoon Index), and DMI (Dipole Mode Index) in the period of January 1998 until August 2010, the results of statistical analysis shows that the ISMI Monsoon index was relatively dominant influence the behavior of rainfall in some areas of western Indonesia. While, DMI did not show a strong correlation coefficient values, and even some areas showed values close to zero. These factors indicate that the Monsoon is still a dominant oscillation is virtually controlled the whole behavior of rainfall in the western region of Indonesia.</description><geographic>Jakarta</geographic><identifier>http://repository.lapan.go.id//lib/phpthumb/phpThumb.php?src=../../images/docs/SNSAA2011.PNG.PNG</identifier><series>Seminar Nasional Sains Atmosfer dan Antariksa 2011</series><description>Hal. 57-66</description><subject>makalah prosiding</subject><recordID>slims-3979</recordID></dc>
|
language |
ind |
format |
Book:Book Book |
author |
Eddy Hermawan |
title |
Peran Data Indeks Monsun Global Dan Iod Terhadap Perilaku Curah Hujan Di Beberapa Kawasan Indonesia |
publisher |
LAPAN |
publishDate |
2011 |
isbn |
9789791458535 |
topic |
Dipole Mode Monsoon Rainfall makalah prosiding |
url |
http://repository.lapan.go.id//index.php?p=show_detail&id=3979 http://repository.lapan.go.id//lib/phpthumb/phpThumb.php?src=../../images/docs/SNSAA2011.PNG.PNG |
contents |
Interactions that occurred between the Monsoon and IOD (Indian Ocean Dipole) are still kept under review, especially its impact on rainfall anomalies that occurred in several regions of Indonesia. Based on the results of the analysis of global Monsoon index of each parameter is represented by ISMI (Indian Summer Monsoon Index), WNPMI (Western North Pacific Monsoon Index), and AUSMI (Australian Monsoon Index), and DMI (Dipole Mode Index) in the period of January 1998 until August 2010, the results of statistical analysis shows that the ISMI Monsoon index was relatively dominant influence the behavior of rainfall in some areas of western Indonesia. While, DMI did not show a strong correlation coefficient values, and even some areas showed values close to zero. These factors indicate that the Monsoon is still a dominant oscillation is virtually controlled the whole behavior of rainfall in the western region of Indonesia. Hal. 57-66 |
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IOS4589.slims-3979 |
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Lembaga Penerbangan dan Antariksa Nasional |
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623 |
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Repositori LAPAN |
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1123 |
collection |
Repositori Institusi LAPAN |
repository_id |
4589 |
subject_area |
The Universe/Alam Semesta, Jagat Raya, Alam Raya, Antariksa, Ruang Angkasa |
city |
JAKARTA TIMUR |
province |
DKI JAKARTA |
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1 |
repoId |
IOS4589 |
first_indexed |
2017-12-09T18:24:52Z |
last_indexed |
2018-01-19T18:20:49Z |
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1686145339511275520 |
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17.205029 |