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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

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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

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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.

Bermawis (ITB)• Dr. Rima

Rachmayani (ITB)• Dr. Eng. Aditya R.

Kartadikaria (ITB)• Dr. rer. nat. Agus

Setiawan (Ministry of Marine Affairs, Indonesia)

• Dr. rer. nat. Mutiara R. Putri (ITB)

• Dr. Dwi Susanto (Maryland University, USA)

• Dr. Augy Syahailatua (LIPI)

Advisory Board

• Prof. Dr. Hasanuddin Z. Abidin (BIG, Indonesia)

• Titiek Suparwati (BIG, Indonesia)

• Prof. Benyamin Sapiie, Ph.D (Dean of FEST, ITB)

• (Dean of FIKP, Hasanuddin University)

• Dr. Antonius Bambang Wijanarto (BIG, Indonesia)

• Ivonne M. Radjawane, M.Si., Ph.D. (ITB)

Organizing Committee

Chair :

• Dr. Ayi Tarya

Members :

• Dr. Eng. Aditya R. Kartadikaria

• Dr. Lamona I. Bernawis• Dr. Rima Rachmayani• Faruq Khadami, M.Si.• Dayu W.

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

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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

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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: [email protected]

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

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MSAT IOP Publishing


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


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),


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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


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


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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


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


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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 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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012001OPEN ACCESS

Ocean numerical model experiment on estimating the variation of volume and heattransport in Karimata straitI P Anwar, M R Putri and A Setiawan


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Evaluation of a global ocean general circulation model; The Lat-Lon-Cap (LLC90)configuration of the MITgcmBernawis Lamona, Judith Hauck and Christoph Völker


012003OPEN ACCESS

The roles of mixed layer depth in affecting chemical and biological characteristics ofMakassar straits, IndonesiaI C Dewi, M R Putri and A Setiawan


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Numerical modeling of wave-current interaction in Merak Port, IndonesiaS Nurfitri, N S Ningsih, A N Sentanu and R Rachmayani


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Environmental assessment of Pari Island towards oil spill using Geographic InformationSystem (GIS): a preliminary studyS Nurfitri, M Raihan, M R Putri, A Setiawan, M Gade and T Pohlmann


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Temperature-Salinity stratification in the Eastern Indian Ocean using argo floatN P Purba, W S Pranowo, I Faizal and H Adiwira


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Monochromatic interfacial wave propagating over one and two bar(s)L H Wiryanto


012012OPEN ACCESS

Numerical simulation of internal wave propagation over a variable topographyR K Yasmin and S R Pudjaprasetya


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Study of coastal flooding in Kupang, East Nusa Tenggara due to Tropical CycloneFrances (case study April 27 – 30 2017)I G A P P Astiduari, T H A Rasyiid and I R Nugraheni

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Analysis of daily wind circulation toward sea level rise in SemarangN Fitrianti, Y D Haryanto, E V S Simamora, H F A Bintari, A Hartoko, S Anggoro and M Zainuri


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Spatial multi criteria approach for tsunami risk assessmentAbu Bakar Sambah, F Miura, Guntur and Fuad


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Identification of Decapterus sp. potential fishing grounds in Java and WesternKalimantan SeasAvrionesti and M R Putri


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Microplastics in Sumba waters, East Nusa TenggaraM R Cordova and U E Hernawan
































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Quantitative assessment of vulnerability in aquaculture: climate change impacts onwhiteleg shrimp (Litopenaeus vannamei) farming in East Java ProvinceA D Puspa, T Osawa and I W Arthana


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Spatial assessment of relative resilience potential to support management of coral reefecosystem in Doreri Bay area, Manokwari Regency, IndonesiaT F Pattiasina, A Sartimbul, B Semedi, E Y Herawati, D D Pelasula, M Krey and Mulyadi


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Chlorophyll-A variability in the southern coast of Java Island, Indian Ocean:corresponding to the tropical cyclone of ErnieU Efendi, A Fadlan and A M Hidayat


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Utilization of AIS (Automatic Identification System) sensor for mobility monitoring offishing vessel based on PFZ (Potential Fishing Zones) distributionS M Purnama, D Y Hutapea and R Permala


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Salt pond analysis using ALOS PALSAR case study Sampang, Madura-IndonesiaS M Purnama, A Cahyawati and D Y Hutapea


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Identification of flood area in the coastal region using remote sensing in KarawangRegency, West JavaBambang Riadi, Baba Barus, Widiatmaka, Moh Yanuar and Bambang Pramudya


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Long term variation of sea level anomaly (September 1992-January 2017) in theIndonesian sea from multi-mission satellite altimetry dataDina A. Sarsito, Kosasih Prijatna, Dudy D. Wijaya, T Nur Fajar, Ivonne M. Radjawane, Wiwin Windupranataand Brian Bramanto


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Oceanographic factors related to Eastern Little Tuna (Euthynnus affinis) catches in thewest Java SeaMega Syamsuddin, Sunarto and Lintang Yuliadi


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Variabilities of the sea level anomalies in the upstream areas of the Kuroshio Current






























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Marine Technology (Sub-theme: Offshore Technology, Underwater Acoustic and OceanObservation)

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Y J Wijaya, S Sugitani, D N Sugianto, D P Wijayanti and Y Hisaki


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Analysis of dissemination methods for remote sensing information in maritime field tosupport the local governmentG D Yudha and S M Purnama


012047OPEN ACCESS

Predictor-corrector scheme for simulating wave propagation on shallow water regionRifky Fauzi and L. Hari Wiryanto


012048OPEN ACCESS

Monitoring remote tidal based on webEngki A Kisnarti and Suryadhi


012049OPEN ACCESS

Stress concentration factor distribution of inclined brace in multiplanar offshore tubulardouble kt jointsRudi Walujo Prastianto, Yoyok Setyo Hadiwidodo, Ibnu Fasyin Fuadi, Mhd Bonar Yudha Prawira Naibaho andPrasetyo Nugroho Rahardianto


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