Teguh Agustiadi

@international.brin.go.id

Research Centre for Oceanography
National Research and Innovation Agency



                 

https://researchid.co/teguhprobuoy

RESEARCH INTERESTS

Physical Oceanography

14

Scopus Publications

410

Scholar Citations

10

Scholar h-index

10

Scholar i10-index

Scopus Publications

  • Field measurements of turbulent mixing south of the Lombok Strait, Indonesia
    R. Dwi Susanto, Zexun Wei, Priyadi Dwi Santoso, Guanlin Wang, Muhammad Fadli, Shujiang Li, Teguh Agustiadi, Tengfei Xu, Bayu Priyono, Ying Li,et al.
    Springer Science and Business Media LLC
    AbstractThe Indonesian seas, with their complex passages and vigorous mixing, constitute the only route and are critical in regulating Pacific–Indian Ocean interchange, air–sea interaction, and global climate events. Previous research employing remote sensing and numerical simulations strongly suggested that this mixing is tidally driven and localized in narrow channels and straits, with only a few direct observations to validate it. The current study offers the first comprehensive temporal microstructure observations in the south of Lombok Strait with a radius of 0.05° and centered on 115.54oE and 9.02oS. Fifteen days of tidal mixing observations measured potential temperature and density, salinity, and turbulent energy dissipation rate. The results revealed significant mixing and verified the remotely sensed technique. The south Lombok temporal and depth averaged of the turbulent kinetic energy dissipation rate, and the diapycnal diffusivity from 20 to 250 m are $$\\varepsilon$$ ε  = 4.15 ± 15.9) × 10–6 W kg–1 and $$K\\rho$$ K ρ = (1.44 ± 10.7) × 10–2 m2s–1, respectively. This $$K\\rho$$ K ρ is up to 104 times larger than the Banda Sea [$$K\\rho$$ K ρ  = (9.2 ± 0.55) × 10–6 m2s–1] (Alford et al. Geophys Res Lett 26:2741–2744, 1999) or the “open ocean” $$K\\rho$$ K ρ = 0.03 × 10–4 m2s−1 within 2° of the equator to (0.4–0.5) × 10–4 m2s−1 at 50°–70° (Kunze et al. J Phys Oceanogr 36:1553–1576, 2006). Therefore, nonlinear interactions between internal tides, tidally induced mixing, and ITF plays a critical role regulating water mass transformation and have strong implications to longer-term variations and change of Pacific–Indian Ocean water circulation and climate.

  • EXTREME UPWELLING EVENTS IN THE SEAS OF THE ALOR KECIL, ALOR ISLAND, INDONESIA
    Anindya Wirasatriya, , Dwi Susanto, Joga Setiawan, Teguh Agustiadi, Iskhaq Iskandar, Aris Ismanto, Arief Laila Nugraha, Ardiansyah Puryajati, Kunarso,et al.
    The Oceanography Society
    Upwelling is a process by which deep, colder, higher-nutrient waters are brought to the sea surface. In the tropics, an indicator that an upwelling event has occurred is lowering of sea surface temperatures (SSTs) to 25°–27°C from a mean of ~28°C. Based on more than one year of in situ data, we observed an unusual extreme upwelling event (EUE) when the near-surface temperature (NST) dropped by 10°C within one hour during the spring tide in Mulut Kumbang Strait of Alor Kecil. The extreme minimum NST during this EUE was ~12°C, and the upward displacement speed of the cold water was ~0.012 m s–1. The increase in salinity from ~30‰ to 34‰–36 ‰ during the decrease in NST indicates a deep source for the cold water mass . From bathymetry and CTD data, the source of the cold water mass was a deep basin (>300 m) located at the southern part of Pantar Strait. In this basin, the temperature at 270 m depth can be as low as 8°C. We suggest that tidal sloshing (i.e., the back-and-forth movement of water) brings the cold water mass through a channel that connects this deep basin to Mulut Kumbang Strait. Interactions between semi-diurnal (M2, S2, and N2) tidal components strongly modulate the tidal signal with a period of nearly one month. That EUEs only occur from August to November also suggests a strong monsoonal influence. Because tides are predictable, we suggest that future EUEs are predictable.

  • Amplitude modulations of seasonal variability in the Karimata Strait throughflow
    Yicong Nie, Shujiang Li, Zexun Wei, Tengfei Xu, Haidong Pan, Xunwei Nie, Yaohua Zhu, R. Dwi Susanto, Teguh Agustiadi, and Mukti Trenggono
    Frontiers Media SA
    The Karimata Strait (KS) throughflow between the South China Sea (SCS) and Java Sea plays an essential role in heat and freshwater budget in the SCS and dual roles in strengthening/reducing the primary Indonesian throughflow (ITF) in the Makassar Strait. A sustained long-term monitoring of the ITF is logistically challenging and expensive; therefore, proxies are needed. Here, we use a combination of in situ measurement of the KS throughflow and satellite-derived sea surface height (SSH) and sea surface wind (SSW) to determine the interannual and decadal modulations in seasonal amplitude of the KS throughflow associated with El Niño-Southern Oscillation (ENSO), Indian Ocean dipole (IOD), Pacific Decadal Oscillation (PDO). Linear regression, correlation, harmonic and power spectrum analyses are used. The results manifest that there are significant interannual to decadal modulations in the seasonal amplitude of the KS throughflow. The modulations of the seasonal amplitude in the volume and heat transports range 1.36-1.92 Sv (1 Sv = 106 m3 s-1) and 126.41-173.36 TW (1 TW = 1012 W), respectively, with a significant cycle of ~9 years. From 1994 to 2020, the seasonal amplitude of volume transport through the KS shows an increasing trend of 37.75 ± 15.69 mSv decade-1 (1 mSv = 103 m3 s-1). The seasonal amplitude of the heat transport also increases, at a rate of 4.78 ± 1.52 TW decade-1. The KS volume transport is positively correlated with PDO and ENSO indices (r2 = 0.69 and r2 = 0.58), with a lag of 12 and 10 months, respectively. The results of composite analysis suggest that the interannual variability of the KS transport is related to the interannual anomalies of the SSH gradient and the local SSW fields in boreal winter.

  • Distributions of Nutrients in Relation to Phytoplankton Community Heterogeneity in the Makassar Strait, Indonesia
    Iis Triyulianti, Agus Setiawan, Faisal Hamzah, Teguh Agustiadi, Bayu Priyono, Mukti Trenggono, and Fithriastuti Nagari
    IOP Publishing
    Abstract The Monitoring of Indonesia Throughflow (MITF) with scientific cruise across the Indonesian waters that are connecting the islands of Kalimantan and Sulawesi or strait of Makassar. This cruise carried out in August 2015 in an area between 2° and 4° South and 118° and 119° East. This cruise aims to characterize the concentration of nutrients and abundance of phytoplankton groups as well as explain their distribution based on the environmental conditions. Nutrient concentrations consisting of Inorganic Dissolved Nitrogen (DIN), Inorganic Dissolved Phosphate (DIP) and Inorganic Dissolved Silicate (DSi) were measured at seven depth layers, i.e. 10, 30-60, 100-150, 300, 500, 750 and 1000 meters. The study showed that in the transitional season (August), the upper layer of study sites were characterized by salinity between 34.05 and 34.76 PSU, temperature between 26.85 and 29.88 °C, and relatively high nutrient concentration, i.e. DIN = 8.91 - 36.74 μM, DIP = 0.02 - 0.16 μM, and DSi= 31.88 - 249.49 μM. The phytoplankton community groups found were Cyanophyta, Bacillariophyta (Diatom), and Dinophyta, where the highest abundance was Cynophyta for the genus Trichodesmium sp. The composition of phytoplankton community in the surface layer is strongly influenced by sea surface temperature, salinity and nutrient concentration. We found that nutrient utilization in the surface layer is relatively high.

  • Satellite-observed multi-scale variability of sea surface chlorophyll-a concentration along the south coast of the sumatra-java islands
    Tengfei Xu, Zexun Wei, Shujiang Li, Raden Dwi Susanto, Nyoman Radiarta, Chao Yuan, Agus Setiawan, Anastasia Kuswardani, Teguh Agustiadi, and Mukti Trenggono
    MDPI AG
    The southern coast of Java is known as one of the most productive fishing grounds for tuna, feeding by nutrient-rich water along the coast caused by the subsurface water upwelling. This primary productivity can be evidenced by the high sea surface chlorophyll-a concentration (SSC). Based on satellite remote sensing products, we investigate the multi-scale variability in SSC along the Sumatra-Java coast. The results show that seasonal variability of SSCs is primarily due to monsoon-driven upwelling and rainfall in the Indian Ocean and Indonesian seas sides of the Sumatra and Java Islands, respectively. Local Ekman pumping plays a secondary role, while rainfall input to the ocean has little effect. Coastally trapped Kelvin waves and mesoscale eddies are responsible for the intraseasonal SSC anomalies in regions along the south coast of Java and off the Sunda and Lombok Straits, respectively. The interannual variability in SSC is caused by the anomalous upwelling related to the Indian Ocean Dipole. There was a weak increasing trend of ~0.1–0.2 mg/m3 per decade, above the global averaged trend, which may be related to enhanced local Ekman pumping. These analyses provide an overall description of SSC variations based on satellite observations; however, further investigations based on in situ observations are needed to achieve better quantification.

  • Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait
    T. F. Xu, Z. X. Wei, R. D. Susanto, S. J. Li, Y. G. Wang, Y. Wang, X. Q. Xu, T. Agustiadi, M. Trenggono, B. Sulistyo,et al.
    American Geophysical Union (AGU)

  • Dynamics of the Carbonate System in the Western Indonesian Seas During the Southeast Monsoon
    Faisal Hamzah, Teguh Agustiadi, R. Dwi Susanto, Zexun Wei, Liguo Guo, Zhimian Cao, and Minhan Dai
    American Geophysical Union (AGU)
    We present a unique water column data set of dissolved inorganic carbon (DIC) and total alkalinity (TAlk) from a cruise to the western Indonesian Seas during the southeast monsoon, covering the Karimata Strait, western Java Sea, and Sunda Strait. Salinity‐normalized TAlk (NTAlk) in the surface water ranged 2,297–2,348 μmol kg, very close to typical values observed in the tropical ocean. In the Karimata Strait, the Kapuas River plume was observed, featuring low salinity, DIC, and TAlk. In the western Java Sea, where waters were well mixed, we observed relatively homogeneous distributions of salinity, DIC, and TAlk. In the Sunda Strait, waters intruding from the Java Sea occupied the upper layer, and below was the Indian Ocean water with lower values of salinity, DIC, and TAlk. In its deep portion, depth profiles of normalized DIC and NTAlk were very similar to those observed in the Indian Ocean. Physical processes and air‐sea gas exchange exerted predominant controls on the carbonate system in the Karimata Strait and western Java Sea. While both processes play large roles in the Sunda Strait, a net DIC removal of 31 ± 23 μmol kg in the surface mixed layer were revealed. The drawdown of DIC is consistent with an overall supersaturation of dissolved oxygen (102–107%), suggesting significant organic carbon production. In the subsurface‐intermediate waters of the Sunda Strait mainly influenced by the advection of Indian Ocean water, a net DIC consumption of 54 ± 45 μmol kg was distinct, likely stimulated by the nutrients supplied from the Indian Ocean. Plain Language Summary Research on the carbonate system in the tropical regime of the Indonesian Seas is minimal, which hampers our understanding to its essential role in interbasin exchanges of material and energy via the Indonesian throughflow. Here we present a unique data set to examine the dynamics of the carbonate system in the western Indonesian Seas. Based on DIC and TAlk relationships, we show that water mass mixing in the western Indonesian Seas during the southeast monsoon is dominated by zonal wind‐mixed waters from the plume of the Kapuas River, the Java Sea and South China Sea mixed water, and the subsurface Indian Ocean water. These processes resulted in homogenous distributions of physical properties and carbonate system parameters. However, biologically mediated DIC consumption occurred in the surface mixed layer of the Sunda Strait, which led to an increase in dissolved oxygen saturation, the saturation state of aragonite (Ωarag), and pH. Overall, our region was a source of atmospheric CO2 as previously reported, although the controlling processes may vary with respect to time at both seasonal and interannual timescales.

  • Makassar Strait Throughflow Seasonal and Interannual Variability: An Overview
    Arnold L. Gordon, Asmi Napitu, Bruce A. Huber, Laura K. Gruenburg, Kandaga Pujiana, Teguh Agustiadi, Anastasia Kuswardani, Nurman Mbay, and Agus Setiawan
    American Geophysical Union (AGU)
    The Makassar Strait throughflow of ~12–13 Sv, representing ~77% of the total Indonesian Throughflow, displays fluctuations over a broad range of time scales, from intraseasonal to seasonal (monsoonal) and interannual scales. We now have 13.3 years of Makassar throughflow observations: November 1996 to early July 1998; January 2004 to August 2011; and August 2013 to August 2017. Strong southward transport is evident during boreal summer, modulated by an ENSO interannual signal, with weaker southward flow and a deeper subsurface velocity maximum during El Niño; stronger southward flow with a shallower velocity maximum during La Niña. Accordingly, the southward heat flux, a product of the along‐channel current and temperature profiles, is significantly larger in summer and slightly larger during La Niña. The southward flow relaxed in 2014 and more so in 2015/2016, similar though not as extreme as during the strong El Niño event of 1997. In 2017, the throughflow increased to ~20 Sv. Since 2016, the deep layer, 300‐ to 760‐m southward transport increases, almost doubling to ~7.5 Sv. Frommid‐2016 into early 2017, the transports above 300 m and below 300 m are about equal, whereas previously, the ratio was about 2.7:1. Near zero or northward flow occurs in the upper 100 m during boreal winter, albeit with interannual variability. Particularly strong winter reversals were observed in 2014/2015 and 2016/2017, the latter being the strongest winter reversal revealed in the entire Makassar time series. Plain Language Summary Pacific water flows into the Indian Ocean within the passages and basins of the Indonesian Seas: the Indonesian Throughflow (ITF), driven by the pressure gradient between the Pacific and Indian Oceans. The ITF affects heat and freshwater inventories of the Pacific and Indian Oceans. The primary inflow path of Pacific water into the Indonesian seas is the Makassar Strait, channeling 12.5 × 10 m/s, about 77% of the total ITF. During the 21 years, November 1996 to August 2017, we have recorded 13.3 years of Makassar throughflow, exposing a broad range of spatial and temporal scale patterns. The Makassar Strait annual cycle transport ranges from about 7 to 16 × 10 m/s. Strong southward transport occurs during boreal summer, with weaker (stronger) southward flow and a deeper (shallower) subsurface velocity maximum during El Niño (La Niña). The throughflow relaxed in 2015 into 2016 during an El Niño. In 2017, the southward transport increased to 20 × 10 m/s. The 300‐ to 760‐m transport increased in 2016 into 2017, equaling the 0‐ to 300‐m transport, from the more typical 30% of the 0‐ to 300‐m transport. Near zero flow occurs in the upper ~100 m during boreal winter with particularly strong winter reversals in 2014/2015 and 2016/2017.

  • Culturable hydrocarbonoclastic marine bacterial isolates from Indonesian seawater in the Lombok Strait and Indian Ocean
    Agung Dhamar Syakti, Priyati Lestari, Satya Simanora, Lilik Kartika Sari, Febrianti Lestari, Fadliyah Idris, Teguh Agustiadi, Syafsir Akhlus, Nuning Vita Hidayati, and Riyanti
    Elsevier BV

  • Seasonal variation of water transport through the Karimata Strait
    Yan Wang, Tengfei Xu, Shujiang Li, R. Dwi Susanto, Teguh Agustiadi, Mukti Trenggono, Wei Tan, and Zexun Wei
    Springer Science and Business Media LLC

  • Monitoring on health condition of tubipora musica (Stolonifera) using colony life-form


  • Observations of intraseasonal variability in the Sunda Strait throughflow
    Shujiang Li, Zexun Wei, R. Dwi Susanto, Yaohua Zhu, Agus Setiawan, Tengfei Xu, Bin Fan, Teguh Agustiadi, Mukti Trenggono, and Guohong Fang
    Springer Science and Business Media LLC

  • Coral reef in center of coral biodiversity (coral triangle): The pulau lirang, southwest moluccas (MBD)


  • Oceanography surrounding Krakatau Volcano in the Sunda Strait, Indonesia
    Dwi Susanto, , Zexun Wei, Rameyo Adi, Quanan Zhang, Guohong Fang, Bin Fan, Agus Supangat, Teguh Agustiadi, Shujiang Li,et al.
    The Oceanography Society

RECENT SCHOLAR PUBLICATIONS

  • Perbandingan Estimasi Stok Karbon Lamun Menggunakan Metode Loss on Ignition (LOI) di Pantai Pejarakan dan Gili Putih Sumberkima, Bali
    AS Abdurohman, LA Assajid, S Hamidah, Z Fahrezi, JM Azriel, D Perta, ...
    MAIYAH 3 (4), 258-276 2024

  • Percampuran Vertikal Turbulen di Perairan Halmahera pada Bulan Oktober 2017
    MS Wahyudi Prasetyo, Wang Zheng, Adi Purwandana, Ashari Wicaksono, Edi ...
    POSITRON 14 (2), 129 - 139 2024

  • Field measurements of turbulent mixing south of the Lombok Strait, Indonesia
    RD Susanto, Z Wei, PD Santoso, G Wang, M Fadli, S Li, T Agustiadi, T Xu, ...
    Geoscience Letters 11 (1), 36 2024

  • Signatures of Oxygen-Depleted Waters along the Sumatra-Java Coasts in the Southeastern Tropical Indian Ocean
    F Hamzah, I Triyulianti, A Setiawan, IS Nurhati, B Priyono, D Berlianty, ...
    EGUsphere 2024, 1-37 2024

  • Distributions of Nutrients in Relation to Phytoplankton Community Heterogeneity in the Makassar Strait, Indonesia
    I Triyulianti, A Setiawan, F Hamzah, T Agustiadi, B Priyono, M Trenggono, ...
    IOP Conference Series: Earth and Environmental Science 1163 (1), 012011 2023

  • Extreme Upwelling Events in the Seas of the Alor Kecil, Alor Island, Indonesia
    A Wirasatriya, RD Susanto, JD Setiawan, T Agustiadi, I Iskandar, ...
    Oceanography 36 (1), 28-37 2023

  • Amplitude Modulations of Seasonal Variability in the Karimata Strait throughflow
    Y Nie, S Li, Z Wei, T Xu, H Pan, X Nie, Y Zhu, RD Susanto, T Agustiadi, ...
    Frontiers in Marine Science 10, 22 2023

  • ALTERNATIF PENGUKURAN KONSENTRASI OKSIGEN TERLARUT DI LAUT INDONESIA BAGIAN BARAT PADA MUSON TENGGARA
    F Hamzah, T Agustiadi, M Trenggono, E Susilo, I Triyulianti
    Jurnal Ilmu dan Teknologi Kelautan Tropis 14 (3), 405-425 2022

  • Overview of Recent Indonesian Throughflow Monitoring and Mixing
    R Susanto, Z Wei, N Hananto, M Fadli, S Li, S Wouthuyzen, P Santoso, ...
    AGU Fall Meeting Abstracts 2021, A54B-01 2021

  • Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait
    TF Xu, ZX Wei, RD Susanto, SJ Li, YG Wang, Y Wang, XQ Xu, T Agustiadi, ...
    Journal of Geophysical Research: Oceans 126 (2), e2020JC016608 2021

  • Satellite-Observed Multi-Scale Variability of Sea Surface Chlorophyll-a Concentration along the South Coast of the Sumatra-Java Islands
    T Xu, Z Wei, S Li, RD Susanto, N Radiarta, C Yuan, A Setiawan, ...
    Remote Sensing 13 (14), 2817 2021

  • Validation of INDO12 Ocean Model at Makassar Strait
    B Priyono, M Trenggono, T Agustiadi
    Omni-Akuatika 16 (2), 83-89 2020

  • Comparison of Simulated and Observed Current Velocities in Karimata and Gaspar Straits
    M Trenggono, B Priyono, RR Hidayat, T Agustiadi
    Omni-Akuatika 16 (3), 42-48 2020

  • TRIUMPH: Transport Indonesian Seas, Upwelling, and Mixing Physics
    RD Susanto, Z Wei, N Hananto, S Wouthuyzen, S Li, H Wang, M Fadli, ...
    AGU Fall Meeting Abstracts 2020, A103-08 2020

  • Dynamics of the carbonate system in the Western Indonesian Seas during the Southeast Monsoon
    F Hamzah, T Agustiadi, RD Susanto, Z Wei, L Guo, Z Cao, M Dai
    Journal of Geophysical Research: Oceans 125 (1), e2018JC014912 2020

  • Makassar Strait throughflow seasonal and interannual variability: An overview
    AL Gordon, A Napitu, BA Huber, LK Gruenburg, K Pujiana, T Agustiadi, ...
    Journal of Geophysical Research: Oceans 124 (6), 3724-3736 2019

  • Culturable hydrocarbonoclastic marine bacterial isolates from Indonesian seawater in the Lombok Strait and Indian Ocean
    AD Syakti, P Lestari, S Simanora, LK Sari, F Lestari, F Idris, T Agustiadi, ...
    Heliyon 5 (5) 2019

  • Seasonal variation of water transport through the Karimata Strait
    Y Wang, T Xu, S Li, RD Susanto, T Agustiadi, M Trenggono, W Tan, Z Wei
    Acta Oceanologica Sinica 38, 47-57 2019

  • Monitoring on health condition of tubipora musica (Stolonifera) using colony life-form
    OM Luthfi, MA Asadi, T Agustiadi, A Soegianto
    Ecology, Environment and Conservation 25 (S), S205-S210 2019

  • Observations of intraseasonal variability in the Sunda Strait throughflow
    S Li, Z Wei, RD Susanto, Y Zhu, A Setiawan, T Xu, B Fan, T Agustiadi, ...
    Journal of Oceanography 74, 541-547 2018

MOST CITED SCHOLAR PUBLICATIONS

  • Makassar Strait throughflow seasonal and interannual variability: An overview
    AL Gordon, A Napitu, BA Huber, LK Gruenburg, K Pujiana, T Agustiadi, ...
    Journal of Geophysical Research: Oceans 124 (6), 3724-3736 2019
    Citations: 110

  • Oceanography surrounding krakatau volcano in the Sunda Strait, Indonesia
    RD Susanto, Z Wei, TR Adi, Q Zheng, G Fang, B Fan, A Supangat, ...
    Oceanography 29 (2), 264-272 2016
    Citations: 62

  • Seasonal variation of water transport through the Karimata Strait
    Y Wang, T Xu, S Li, RD Susanto, T Agustiadi, M Trenggono, W Tan, Z Wei
    Acta Oceanologica Sinica 38, 47-57 2019
    Citations: 43

  • Observed Water Exchange Between the South China Sea and Java Sea Through Karimata Strait
    TF Xu, ZX Wei, RD Susanto, SJ Li, YG Wang, Y Wang, XQ Xu, T Agustiadi, ...
    Journal of Geophysical Research: Oceans 126 (2), e2020JC016608 2021
    Citations: 29

  • Satellite-Observed Multi-Scale Variability of Sea Surface Chlorophyll-a Concentration along the South Coast of the Sumatra-Java Islands
    T Xu, Z Wei, S Li, RD Susanto, N Radiarta, C Yuan, A Setiawan, ...
    Remote Sensing 13 (14), 2817 2021
    Citations: 27

  • Dynamics of the carbonate system in the Western Indonesian Seas during the Southeast Monsoon
    F Hamzah, T Agustiadi, RD Susanto, Z Wei, L Guo, Z Cao, M Dai
    Journal of Geophysical Research: Oceans 125 (1), e2018JC014912 2020
    Citations: 25

  • Observations of intraseasonal variability in the Sunda Strait throughflow
    S Li, Z Wei, RD Susanto, Y Zhu, A Setiawan, T Xu, B Fan, T Agustiadi, ...
    Journal of Oceanography 74, 541-547 2018
    Citations: 24

  • Culturable hydrocarbonoclastic marine bacterial isolates from Indonesian seawater in the Lombok Strait and Indian Ocean
    AD Syakti, P Lestari, S Simanora, LK Sari, F Lestari, F Idris, T Agustiadi, ...
    Heliyon 5 (5) 2019
    Citations: 22

  • Coral Reef in Center of Coral Biodiversity (Coral Triangle): The Pulau Lirang, Southwest Moluccas (MBD)
    OM Luthfi, MA Asadi, T Agustiadi
    Disaster Advances 9 (Vol. 11(9) September 2018), 1-7 2018
    Citations: 13

  • Analisis diagram TS berdasarkan parameter oseanografis di perairan selat Lombok
    L Harvianto, M Parengkuan, AF Koropitan, T Agustiadi
    Journal of Technology 1 (1), 101-117 2015
    Citations: 13

  • Pemantauan Elevasi Muka Air Selat Bali dengan Menggunakan Stasiun Pasang Surut
    M Trenggono, B Priyono, T Agustiadi, MA Rahman, G Putu
    Research Gate, 39-47 2015
    Citations: 6

  • Diversity of stoloniferan coral (Stolonifera) at Lirang Island, Southwest Maluku (Moluccas), Indonesia
    T Agustiadi, OM Luthfi
    International Journal of Oceans and Oceanography 11 (1), 21-30 2017
    Citations: 5

  • Observasi karakteristik perairan Selat Bali melalui pendekatan insitu dan numerik
    WER Siwi, B Priyono, T Agustiadi
    Bunga Rampai Observasi Oseanografi di Indonesia, 13-25 2015
    Citations: 5

  • Struktur Komunitas Plankton di Perairan Selat Bali
    T Agustiadi, F Hamzah, M Trenggono
    Omni Akuatika 17 (XII), 72-79 2013
    Citations: 5

  • Riyanti (2019) Culturable hydrocarbonoclastic marine bacterial isolates from Indonesian seawater in the Lombok Strait and Indian Ocean. Heliyon 5 (5): e01594
    AD Syakti, P Lestari, S Simanora, LK Sari, F Lestari, F Idris, T Agustiadi, ...
    Citations: 5

  • Extreme Upwelling Events in the Seas of the Alor Kecil, Alor Island, Indonesia
    A Wirasatriya, RD Susanto, JD Setiawan, T Agustiadi, I Iskandar, ...
    Oceanography 36 (1), 28-37 2023
    Citations: 3

  • Validation of INDO12 Ocean Model at Makassar Strait
    B Priyono, M Trenggono, T Agustiadi
    Omni-Akuatika 16 (2), 83-89 2020
    Citations: 3

  • Monitoring on health condition of tubipora musica (Stolonifera) using colony life-form
    OM Luthfi, MA Asadi, T Agustiadi, A Soegianto
    Ecology, Environment and Conservation 25 (S), S205-S210 2019
    Citations: 3

  • Field measurements of turbulent mixing south of the Lombok Strait, Indonesia
    RD Susanto, Z Wei, PD Santoso, G Wang, M Fadli, S Li, T Agustiadi, T Xu, ...
    Geoscience Letters 11 (1), 36 2024
    Citations: 2

  • Amplitude Modulations of Seasonal Variability in the Karimata Strait throughflow
    Y Nie, S Li, Z Wei, T Xu, H Pan, X Nie, Y Zhu, RD Susanto, T Agustiadi, ...
    Frontiers in Marine Science 10, 22 2023
    Citations: 1