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LEMBAR HASIL PENILAIAN SEJA WAT SEBIDANG ATAU PEER REVIEW
KARYA ILMIAH : PROSIDING C32.
Judul Karya Ilmiah Jumlah Penulis Status Pengusul Identitas Prosiding
Variabilities of the sea level anomalies in the upstream areas of the Kuroshio Current 5 Orang (Y J Wijaya, S Sugitani, D N Sugianto, D P Wijayanti, and Y Hisaki) Penulis ke-4 a. Judul Prosiding
b. ISBN/lSSNc. Thn Terbit, Tempat Pelaks.d. Penerbit/Organisere. Alamat Repository/Web
Alamat Artikel
f. Terindeks di (jika ada)
1st International Conference on Maritime Sciences and Advanced Technology "Ocean Science and Technology Toward a Global Maritime Axis" IOP Conf. Series: Earth and Environmental Science (2018)
2018, IOP Publisher https://iopscience.iop.org/article/1 0. l 088/1755-1315/162/l/0 12045 http://iopscience.iop.org/article/ l 0.1088/1755-l 315/162/1/012045/pdfScopus
Kategori Publikasi Makalah (beri / pada katego · yang tepat)
: []] Prosiding Forum Ilmiah Intemasional D Prosiding Forum Ilmiah Nasional
Hasil Penilaian Peer Review
Komponen Yang Dinilai
a. Kelengkapan unsur isi prosiding (10%)b. Ruang lingkup dan kedalaman pembahasan
(30%)C. Kecukupan dan kemutahiran data/informasi dan
metodologi (30%)d. Kelengkapan unsur dan kualitas terbitan
/prosiding (30%)Total = (100%)
Semarang, Reviewer 1
Prof. Dr. Ir. Supriharyono, M.Sc NIP 195007151978021001 Unit Kerja: FPIK UNDIP
Nilai Reviewer Nilai Rata -
Rata Reviewer 1 Reviewer2
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Reviewer 2
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Prof. Dr. Ir. Slamet Budi Prayitno, M.Sc NIP. 1955062819815031005 Unit Kerja : FPlK UNDIP
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IOP Conference Series: Earth and Environmental ScienceScopus coverage years: from 2010 to PresentISSN: 1755-1307 E-ISSN: 1755-1315Subject area: Earth and Planetary Sciences: General Earth and Planetary Sciences
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https://fitb.itb.ac.id/event/1st-international-conference-on-mariteme-science-and-advanced-technology-msat/
HOME PROGRAM REGISTRATION VENUE & ACCOMODATION
PREVIOUS EVENT
Scientific Committee
• Prof. Hasanuddin Z. Abidin (BIG)
• Zhejiang University• Prof. LI
Chunfeng (Zhejiang University)
• Dr. Agus Santoso (UNSW, Australia)
• Dr. Hamzah Latief (ITB)• Dr. Eng. Nining Sari
Ningsih (ITB)• Dr. Ibnu Sofian (BIG,
Indonesia)• Dr. Lamona I.
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Rachmayani (ITB)• Dr. Eng. Aditya R.
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• Dr. Augy Syahailatua (LIPI)
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• Prof. Dr. Hasanuddin Z. Abidin (BIG, Indonesia)
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• Prof. Benyamin Sapiie, Ph.D (Dean of FEST, ITB)
• (Dean of FIKP, Hasanuddin University)
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Purnaningtyas, M.Si.• Farrah Hanifah M.Si.• Karina A. Sujatmiko, M.T.• Faizal Ade, M.Si.• Annisa Martina, M.Si.• Hanif Santyabudi, M.Sc.• Iwan P. Anwar, M.Si.• Ardian Mahiru Rizal, S.Si.• Umar Abdurahman, S.Si.
Committee
1
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Published under licence by IOP Publishing Ltd
1234567890 ‘’“”
MSAT IOP Publishing
IOP Conf. Series: Earth and Environmental Science 162 (2018) 012002 doi :10.1088/1755-1315/162/1/012002
Evaluation of a global ocean general circulation model; The
Lat-Lon-Cap (LLC90) configuration of the MITgcm
Bernawis Lamona1, Judith Hauck2 and Christoph Völker2
1Department of Oceanography, Institut Teknologi Bandung, Indonesia 2Alfred Wegener Institute, Germany
E-mail: lamona@fitb.itb.ac.id
Abstract. An evaluation of a general circulation model from Massachusetts Institute of
Technology (MITgcm) with Lat – Lon – Cap (LLC90) configuration was done. Simulation of
100 years yields the annual means of potential temperature, salinity, meridional overturning
stream function and transport of several throughflows. A reference run with widened Davis
strait from the model was used to compare with observational WOA09 data, and the MITgcm
has reproduced reasonably reliable data. The patterns of potential temperature can resemble the
WOA09, however not so for the salinity fields. An experiment to simulate the model in 5
different tuning set were then proceeded. For the potential temperature and salinity fields, the
North Pacific and the Southern Ocean still has significant difference to the WOA09. The
difference was in the range of -6 to 5 ⁰C for the potential temperature and -0.5 to 3 psu for the
salinity field. The meridional overturning circulation stream function was still lower than the
observational (± 17 Sv); the MITgcm simulates it 10 ± 1Sv in the experiment. The root mean
square (RMS) of the difference were calculated, the surface layer has the largest magnitude of
difference due to the forcing dynamics. The best simulation, which has the least difference to
WOA09, was the one with the original bathymetry and smallest vertical diffusivity coefficient,
1 x 10-5 m2 s-1.
1. Introduction
MITgcm is widely used by oceanographers in wide spectrum of expertise; physics, biology, chemistry,
and ocean-atmosphere interactions among others. The uniqueness of this general circulation model is
that it employs the non-hydrostatic equation and fluid isomorphism to simulate fluid phenomena of
both ocean and atmosphere, from the small scale of convection with 100m range to the general
circulation of the world ocean on a scale of thousands of kilometers. In our simulations we used a
resolution of 1⁰. Marshall [1] elaborated ocean models based on hydrostatic primitive equations (HPE), quasi
hydrostatic (QH) and non-hydrostatic (NH) equations. In HPE, the vertical momentum equation is
reduced to hydrostatic balance and an approximation is made with approximated Coriolis force and a
shallow atmosphere approximation is made. With this, in large scale, the terms omitted in HPE are
negligible, but on a small scale they become large enough to become a problem. For the application to
1
Content from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distributionof this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.
Published under licence by IOP Publishing Ltd
1234567890 ‘’“”
MSAT IOP Publishing
IOP Conf. Series: Earth and Environmental Science 162 (2018) 012031 doi :10.1088/1755-1315/162/1/012031
Effects of artificial and natural materials ropes as
substrates for settling and metamorphosis of pediveliger
pearl oyster, Pinctada maxima (Jameson, 1901)
Medy Ompi1, Fontje Kaligis1, Stephanus Mandagi1, and Kathe Jensen2
1Department of Natural Water Resources Management, Faculty of Fisheries and
Marine Sciences University of Sam Ratulangi, Indonesia 2Zoologisk Museum, Copenhagen, Denmark
E-mail: ompimedy@unsrat.ac.id
Abstract. A study aimed at investigating the effects of four different materials ropes as
substrates for settling and metamorphosis of tropical oyster, Pinctada maxima,
pediveligers was conducted at laboratory scale. The number of pediveligers attached and
metamorphosed on each substratum were counted at the terminat ion of the experiment.
Increment in shell length during settling and metamorphosis was also measured. Settling
and metamorphosis were analyzed using One-Way ANOVA with substratum as the main
effect. Two-Way ANOVA with time and substratum as the main effect on growth was
also tested. The results showed that the settling and metamorphosis of pediveliger were
affected by the substratum. The number of settled and metamorphosed pediveligers on
polypropylene rope, natural ropes of Arenga piñata and Cocos nucifera was significantly
higher than on the bottom of Pyrex glasses. No significant difference between numbers of
larvae settled on polypropylene and natural ropes of Arenga piñata and Cocos nucifera
appeared. A significant effect of time, but not of substratum, on growth occurred.
Overall, settling and metamorphosis of P. maxima pediveliger larvae were strongly
affected by artificial and natural ropes, while metamorphosis occurred haphazardly on the Pyrex glass. Growth occurred after settling and metamorphosis.
1. Introduction
Pearl oysters, Pinctada maxima (Jameson, 1901), have been actively cultured and developed to be the
main pearl oyster industry in North Sulawesi. Spat of this pearl oyster is mainly supplied from
hatcheries or collected from the oyster bed using spat collectors. Nowadays the use of polypropylene
and monofilament as substrate for spat collectors has been intensified. Yet the unused materials are
being dumped into the sea and become wastes, affecting benthic organisms as it may be ingested,
accumulated and possibly transferred to higher throphic levels. According to Chae & Joo An (2017),
1
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Published under licence by IOP Publishing Ltd
1234567890 ‘’“”
MSAT IOP Publishing
IOP Conf. Series: Earth and Environmental Science 162 (2018) 012033 doi :10.1088/1755-1315/162/1/012033
Depositional environmental evolution of Kalibiuk formation based on paleontological molluscan Study, Cisaat River section, Bumiayu, Central Java, Indonesia
Aswan1, Elina Sufiati2, Alfend Rudyawan1, Desty Kistiani2, and Thaw Zin Oo3
1 Geology Department, Faculty of earth Sciences and Technology, Institute of Technology Bandung, Jalan Ganesa 10 Bandung, Indonesia 2 Geological Museum Bandung, Jalan Diponegoro No.57, Bandung, Indonesia 3 Geology Department, East Yangon University, Thanlyin Township, Yangon Division, Myanmar
E-mail: aswan_gl@gl.itb.ac.id
Abstract. This paper presents new finding from the sedimentary sequences, overlooked by previous researchers, which provide insights to the sea level changes during the deposition of the Middle to Late Pliocene Kalibiuk Formation. Data were acquired from fieldwork via detailed measured section of each sedimentary sequence from the bottom to the upper part of the formation followed by molluscan fossil association analyses. Lithologically, the Cisaat River stratigraphic section is dominated by greenish grey claystone with some light grey fine-grained sandstone intercalation. Based on about 50 m stratigraphic section, 10 molluscan fossils associations were successfully determined. The sequence from bottom to top are: Corbula– Natica association, Nassa sp. association, Olividae – Turricula association, Pecten – Telina association, Telina – Placuna association, Corbula – Marginella association, Placuna – Natica association, Turritella association, Turritella – Marginella association and Dentalina – Architectonica association. Changes in vertical succession of the molluscan association indicates a development from shallow marine to terrestrial depositional environment before gradually overlain by terrestrial sediments of the Kaliglagah Formation. At least there are 2 deepening - shallowing sea level cycles during the deposition of Kalibiuk Formation observed from this section.
1. IntroductionThe Cisaat River traverse is located to the southwest of Bumiayu, Central Java, Indonesia (Figure 1).Standard geological map of the area referred to the Majenang sheet [1], bounded by the followingcoordinates: 7º 09’ 20.55” S; 108º 57’ 13.41” E - 7º 09’ 34.53” S; 108º 57’ 21.76” E. The traverse,administratively, belong to the Bantarkawung district, Brebes, Central Java Province. This study focuses on the upper part of the Pliocene Kalibiuk Formation [1] and the lower part of the Pleistocene Kaliglagah Formation (Figure 2) with general bedding attitude N060°E/30°SE. This interval is included into the Cheribonian stage in the Neogene stages of Jawa [2] based on the mollusc fossils occurrence or the Zanclian stage in the international geological time scale. This research was carried out due to the abundance and continuous occurrence of marine mollusc fossils across the vertical succession of the formation along the traverse and rare occurrence of benthic forams that are usually used to determine
1
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Published under licence by IOP Publishing Ltd
1234567890 ‘’“”
MSAT IOP Publishing
IOP Conf. Series: Earth and Environmental Science 162 (2018) 012038 doi :10.1088/1755-1315/162/1/012038
Estimation of marine gravity anomaly model from satellite
altimetry data (Case Study : Kalimantan and Sulawesi
Waters-Indonesia)
P Hartanto1, S Huda1, W Putra1, E D Variandy1, B Triarahmadhana1, D
Pangastuti1, A M Pahlevi1 and C Hwang2
1 Geospatial Information Agency of Indonesia, Jl. Raya Jakarta-Bogor Km. 46,
Cibinong 16911, West Java, Indonesia 2 National Chiao Tung University, 1001 University Road, Hsinchu, Taiwan 300, ROC
E-mail: hartantoprayudha@gmail.com
Abstract. Nowadays satellite altimetry has become an advanced instrument to observe many
natural physical phenomena, such as sea-level rise, ocean circulation, water mass changes, and
marine gravity anomaly. The use of satellite altimetry data to compute marine gravity anomaly
provides good results and costs relatively low. Those advantages make geodesists utilize this
method as an alternative in geoid determination, especially over the seas. Several sets of satellite
altimetry data from Cryosat 2, Jason 1 phase C, Geosat and ERS1 were used to compute gravity
anomaly over the surrounding waters of Kalimantan and Sulawesi Island in Indonesia. The study
area spans between -70-70 N and 1080-1270 E with a spatial resolution of 1’x1’. In the pre-
processing step, the altimetry data especially Geosat and ERS1, were retracked to reduce errors
due to the land influence. The main computation step was done by using two different methods,
least square collocation (LSC) and Inverse Vening-Meinesz (IVM). The computed gravity
anomaly models then assessed with the in-situ marine gravity data from the National
Geophysical Data Center (NGDC). The best model in term of RMS error is the 10 km Gaussian
filtered LSC with an RMS error of 15.042 mgal. The least accurate model is the non-filtered IVM with an RMS of 16.704 mgal.
1. Introduction
The Kalimantan and Sulawesi are two main islands of Indonesian Archipelago. In order to determine
the regional geoid, the government of Indonesia in collaboration with Technical University of Denmark
(DTU) ran airborne gravity surveys over those two Islands in 2008-2009 [1]. However, the surveys did
not cover the waters surrounding those two islands [2]. In order to fill those gaps, some geodetic mission
altimetry datasets were used to determine the gravity anomalies over an area between 7⁰S - 7⁰ N and
108⁰E - 127⁰E. The datasets consist of Sea Surface Height (SSH) measured by Cryosat-2, Jason-1 phase
C, Geosat and ERS-1 satellite altimetry missions. By definition, SSH is the difference of altimeter range
from the satellite altitude above the reference ellipsoid [3], or in another word SSH is the height of
instantaneous sea surface above the reference ellipsoid.
To make the SSH data usable in gravity anomaly determination, some accuracy defects related to
land occurrence should be reduced by performing waveform retracking. Waveform retracking was
performed to fit a model or functional form to the measured waveforms, and retrieve geophysical
8/1/2019 IOP Conference Series: Earth and Environmental Science, Volume 162, 2018 - IOPscience
https://iopscience.iop.org/issue/1755-1315/162/1 1/8
Table of contents
View all abstracts
Accepted papers received: 5 June 2018Published online: 6 July 2018
Preface
Papers
Ocean and Coastal Dynamics
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1st International Conference on Maritime Sciences and Advanced Technology "OceanScience and Technology Toward a Global Maritime Axis"3–5 August 2017, Denpasar, Bali, Indonesia
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1st International Conference on Maritime Sciences and Advanced Technology "OceanScience and Technology Toward a Global Maritime Axis"
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8/1/2019 IOP Conference Series: Earth and Environmental Science, Volume 162, 2018 - IOPscience
https://iopscience.iop.org/issue/1755-1315/162/1 8/8
Marine Technology (Sub-theme: Offshore Technology, Underwater Acoustic and OceanObservation)
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