Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali

<p>DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v8i3.161" target="_blank">10.17014/ijog.v8i3.161</a></span></p><p>Sea surface salinity is an important parameter in a climate study. Coral δ18O records δ18O seawater and sea surface t...

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Main Author: Sri Yudawati Cahyarini
Format: Article
Language:English
Published: Geological Agency 2014-07-01
Series:Indonesian Journal on Geoscience
Subjects:
SST
Online Access:https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/161
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spelling doaj-55af5d7bae734c1c94e9f41fedec1da82020-11-25T01:26:02ZengGeological AgencyIndonesian Journal on Geoscience2355-93142355-93062014-07-018311912510.17014/ijog.8.3.119-125161Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and BaliSri Yudawati Cahyarini0Pusat Penelitian Geoteknologi - LIPI Jln. Sangkuriang Bandung<p>DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v8i3.161" target="_blank">10.17014/ijog.v8i3.161</a></span></p><p>Sea surface salinity is an important parameter in a climate study. Coral δ18O records δ18O seawater and sea surface temperature (SST). While, coral Sr/Ca records SST only commonly used in a paleoclimate study to reconstruct SST. Thus, paired coral δ18O and Sr/Ca can be used to reconstruct δ18O seawater. δ18O seawater and SSS is linearly correlated, thus reconstructed δ18O seawater further is used to reconstruct sea surface salinity (SSS). Instead of using coral Sr/Ca as SST recorder, paired model (grid) or measured SST data is used to reconstruct SSS. In this study, paired coral δ18O and grid SST data are presented to reconstruct SSS from several different locations across Indonesian sea i.e Simeulue, Mentawai, Bunaken, and Bali. Coral-based SSS reconstructions from those locations are then compared to the grid SSS in the seasonal mean scale. The result shows that annual mean variation of salinity for period of 1958-2008 in Mentawai and Simeulue is 33.25 psu and 33.26 psu respectively, while in Bunaken and Bali is 34.03 psu and 33.47 psu respectively. Correlation coefficient between coral salinity and salinity from model data in the seasonal/monthly mean scale is high i.e R = 0.62 - 0.83. Based on the monthly mean data, corals in the studied area strongly record SSS variation in the monthly or seasonal mean scale. In Mentawai and Simeulue waters, SSS variation is influenced strongly by monsoon. While, in addition to the monsoon, ocean advection also affects seasonal variability of SSS in the Bunaken and Bali waters.<br /><br /></p>https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/161salinitycoralδ18OSSTSimeulueMentawaiBunakenBali
collection DOAJ
language English
format Article
sources DOAJ
author Sri Yudawati Cahyarini
spellingShingle Sri Yudawati Cahyarini
Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
Indonesian Journal on Geoscience
salinity
coral
δ18O
SST
Simeulue
Mentawai
Bunaken
Bali
author_facet Sri Yudawati Cahyarini
author_sort Sri Yudawati Cahyarini
title Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
title_short Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
title_full Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
title_fullStr Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
title_full_unstemmed Seasonal Mean Variability of Coral-based Sea Surface Salinity from Simeulue, Mentawai, Bunaken, and Bali
title_sort seasonal mean variability of coral-based sea surface salinity from simeulue, mentawai, bunaken, and bali
publisher Geological Agency
series Indonesian Journal on Geoscience
issn 2355-9314
2355-9306
publishDate 2014-07-01
description <p>DOI: <span><a href="http://dx.doi.org/10.17014/ijog.v8i3.161" target="_blank">10.17014/ijog.v8i3.161</a></span></p><p>Sea surface salinity is an important parameter in a climate study. Coral δ18O records δ18O seawater and sea surface temperature (SST). While, coral Sr/Ca records SST only commonly used in a paleoclimate study to reconstruct SST. Thus, paired coral δ18O and Sr/Ca can be used to reconstruct δ18O seawater. δ18O seawater and SSS is linearly correlated, thus reconstructed δ18O seawater further is used to reconstruct sea surface salinity (SSS). Instead of using coral Sr/Ca as SST recorder, paired model (grid) or measured SST data is used to reconstruct SSS. In this study, paired coral δ18O and grid SST data are presented to reconstruct SSS from several different locations across Indonesian sea i.e Simeulue, Mentawai, Bunaken, and Bali. Coral-based SSS reconstructions from those locations are then compared to the grid SSS in the seasonal mean scale. The result shows that annual mean variation of salinity for period of 1958-2008 in Mentawai and Simeulue is 33.25 psu and 33.26 psu respectively, while in Bunaken and Bali is 34.03 psu and 33.47 psu respectively. Correlation coefficient between coral salinity and salinity from model data in the seasonal/monthly mean scale is high i.e R = 0.62 - 0.83. Based on the monthly mean data, corals in the studied area strongly record SSS variation in the monthly or seasonal mean scale. In Mentawai and Simeulue waters, SSS variation is influenced strongly by monsoon. While, in addition to the monsoon, ocean advection also affects seasonal variability of SSS in the Bunaken and Bali waters.<br /><br /></p>
topic salinity
coral
δ18O
SST
Simeulue
Mentawai
Bunaken
Bali
url https://ijog.geologi.esdm.go.id/index.php/IJOG/article/view/161
work_keys_str_mv AT sriyudawaticahyarini seasonalmeanvariabilityofcoralbasedseasurfacesalinityfromsimeuluementawaibunakenandbali
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