scholarly journals Physical Oceanography Condition in Eastern Karimata Strait: Pasir Mayang Beach West Kalimantan

2018 ◽  
Vol 8 (1) ◽  
pp. 51
Author(s):  
Harianto Harianto ◽  
Arie Antasari Kushadiwijayanto ◽  
Apriansyah Apriansyah
Keyword(s):  
Current Velocity ◽  
High Tide ◽  
Physical Oceanography ◽  
Wave Direction ◽  
West Kalimantan ◽  
Wave Measurement ◽  
Tidal Data ◽  
Average Current ◽  
Propagation Medium ◽  
Karimata Strait

Karimata strait is located in the western Indonesian, separate the Kalimantan and Belitung island, that has an important role for the distribution services. The information about its dynamics such as tidal behavior, and wave is the key to support the navigation activities in this area. This research describes the results of measurements of the physical oceanography parameter on the eastern side of the Karimata Strait, Pasir Mayang Beach. The tidal data were measured for 15 days in February 25th – March 12th, 2017 and sea current were observed for 24 hours on February 27-28th, 2017. The result showed that tidal type in this area is diurnal tide with amplitude of M2, S2, K1, and O1 respectively are 0.085 m, 0.086 m, 0.455 m, and 0.342 m. Significant wave’s high is ranged from 0.12 – 0.31 m with significant period of 5.32-6.9 s. The wave direction is south western. The current velocity is ranged from 0.087- 0.112 m/s and average current velocity is 0.092 m/s. The tidal current direction is northeast at low tide and south western at high tide. This study also reveals important information that wave energy variability is not only affected by seasonal conditions but also influenced by tides. The tides have responsibility to change the propagation medium of wave that is originated dispersive to non-dispersive medium. This study opens a new study of correction of wave measurement procedures by including and taking into account the effects of tides.

scholarly journals Tidal, wave, current and sediment flow patterns in wet season in the estuary of Porong River Sidoarjo, Indonesia

2018 ◽  
Vol 177 ◽  
pp. 01016
Author(s):  
A. Kisnarti Engki ◽  
Dj. Prasita Viv
Keyword(s):  
Flow Patterns ◽  
Current Data ◽  
Tidal Wave ◽  
Physical Oceanography ◽  
Sediment Thickness ◽  
Wet Season ◽  
The West ◽  
Tidal Current Velocity ◽  
Tidal Data ◽  
Sediment Flow

The objectives of this research are to analyze characteristics of physical oceanography, such as : tides, waves, currents, and discharges at Muara Kali Porong. This research also discuss sediment flow patterns and morphology in around the Estuary of Porong River. Tidal data were used as correction to the depth. The calculation to determine the tidal current velocity and wind data along with current data are used for simulation model. Sedimentation process with a simulation of 15 days in the West Season occured in the Northeast of Lusi Island with sediment thickness ranged from 1.6 to 2.6 m.

scholarly journals Kajian Pola Arus Laut dan Distribusi Sedimen Di Perairan Pantai Muara Kamal Jakarta Utara

2018 ◽  
Vol 1 (1) ◽  
Author(s):  
Permana Ari Soerjawo ◽  
Thonas Indra Maryanto
Keyword(s):  
Current Velocity ◽  
High Tide ◽  
Clay Fraction ◽  
Secondary Data ◽  
Acoustic Doppler Current Profiler ◽  
Google Earth ◽  
Ocean Current ◽  
Primary Data ◽  
Sediment Distribution ◽  
Current Profiler

ABSTRAKPola arus laut dan distribusi sedimen merupakan proses dinamika di suatu perairan yang mempunyai karakteristik berbeda-beda, sehingga berpengaruh terhadap pembentukan geomorfologi pantai di seluruh dunia. Penelitian ini bertujuan untuk mengetahui pola arus dan sedimen di perairan Pantai Muara Kamal Jakarta Utara di tahun 2012. Data yang digunakan merupakan data primer dan data sekunder, data primer meliputi data arus yang didapat dari pemasangan ADCP(Acoustic Doppler Current Profiler), data pasang surut dan sedimen perairan yang diambil dengan sedimen grab. Data sekunder berupa peta LPI (Lingkungan Pantai Indonesia) tahun 2000 skala 1:50.000 dari BIG (Badan Informasi Geospasial) dan citra satelit Google Earth tahun 2009. Hasil penelitian menunjukan bahwa kecepatan arus yang paling besar terdapat pada lapisan permukaan dengan kecepatan 0,242 m/s kearah barat daya (207,8o), kecepatan arus terkecil terdapat pada lapisan dasar yaitu 0,141 m/s kearah barat daya (207o). Hasil simulasi model hidrodinamika 2D, menunjukkan bahwa pada saat pasang arus laut mengarah ke daratan (selatan) dan pada saat surut arus laut mengarah ke laut lepas (barat laut). Berdasarkan kandungan ukuran butir sedimen di perairan Pantai Muara Kamal Jakarta Utara adalah pasir (64.98 - 72.15%) fraksi pasir tertinggi distasiun B(belakang geotekstil), lanau (24.56 - 29.36%) fraksi lanau tertinggi di stasiun C (depan geotekstil) dan Lempung (1.64 – 5.64%) fraksi lempung tertinggi di stasiun C (depan geotekstil). Kata kunci: Arus, Pantai Muara Kamal, Sedimen, model hidrodinamika 2D   ABSTRACTOcean current and sediment distribution are the dynamic process that have different charactheristic and therefore influenced beach geomorfophology around the world. This research aims to understand both ocean current and sediment pattern in Muara Kamal North Jakarta in 2012. This research used primary and secondary data, primary data were consisted of current data from ADCP (Acoustic Doppler Current Profiler), tidal data and bottom sediment samples. Secondary data involved of Indonesia Coastline Environmental map of year 2000 with scale 1:50.000 from Geospatial information Agency and a satellite data from Google earth of year 2009. The results showed that greatest ocean current velocity contained in the surface layer at a speed of 0,242 m/s with to southwest direction (207.8o), the smallest current velocity was in bottom layer is 0.141 m/s with southwest directiont (207o). Based on 2D hydrodynamic model simulation indicated that when high tide ocean current was flowed to the mainland (south) when low tide the current was flowed to the open sea direction. Based on the content grain size of the sediment, the studi area consisted of sand (64.98 - 72.15%) the highest sand fraction at station B(rare of geotextile) , silt (24.56 - 29.36%) the highest silt fraction at station C (front of geotextile) andclay (1.64 – 5.64%) the highest clay fraction at station C(front of geotextile) Key Words: Current, Muara Kamal Shoreline, Sediment, 2D hydrodynamics model

scholarly journals The hydrodynamics condition of water operating area for flight test site selection of N219 Amphibious aircraft

2021 ◽  
Vol 930 (1) ◽  
pp. 012056
Author(s):  
H Khoirunnisa ◽  
M Wibowo ◽  
W Hendriyono ◽  
K S Wardani
Keyword(s):  
Site Selection ◽  
Flight Test ◽  
Test Site ◽  
Water Area ◽  
Surface Elevation ◽  
Wave Direction ◽  
Tidal Data ◽  
Average Water ◽  
Bathymetric Map ◽  
Selection Of

Abstract This research aims to assess the hydrodynamics condition of the water area for site selection of that purpose. The bathymetry data of Karimunjawa Island were obtained from the 1986 Pushidrosal bathymetric map. Furthermore, wind direction, wind speed, wave height and direction, and tidal data around the waters of Karimunjawa Island were input in hydrodynamic and spectral modelling using MIKE 21 HD-SW. West monsoon and east monsoon were applied in this model. The validation result between hydrodynamic modelling and Tidal Model Driver (TMD) data is 98.89%. The surface elevation around the domain has a range of 0.072 - 0.5 m. The average water depth at the seaplane dock plan is about 2.5 m from MSL. The hydrodynamic modeling results show that the surface elevation value at the seaplane dock plan location shows that the sea level is between -0.467 to 0.473 m (in both west and east season). The current velocity at the planned seaplane dock site in both the west and east monsoons is relatively slow (<0.185 m/s). The dominant wave direction is southeastward in the east and west monsoons. The dominant Hs is about 0.23 – 0.6 m in both seasons. At the planned water operating area, the average of Hs is 0.23 m - 0.36 m. Generally, this location fulfills the criteria of site selection for the flight test location of N219A.

scholarly journals Pengaruh Hidrotopografi dan Peruntukan Lahan Terhadap Saluran Tersier Daerah Rawa Pinang Dalam

2020 ◽  
Vol 20 (01) ◽  
pp. 1-10
Author(s):  
Henny Herawati ◽  
Eko Yulianto ◽  
Azmeri
Keyword(s):  
Land Use ◽  
Agricultural Land ◽  
Water System ◽  
Secondary Data ◽  
Primary Data ◽  
Rooting Depth ◽  
West Kalimantan ◽  
Tidal Data ◽  
Optimum Depth ◽  
Level Elevation

[ID] Daerah Rawa Pinang Dalam merupakan bagian dari daerah rawa di kawasan Pinang Komplek yang berada di Kabupaten Kubu Raya Provinsi Kalimantan Barat. Tinggi muka air tanah Daerah Rawa Pinang Dalam dipengaruhi oleh pasang surut air laut. Daerah Pinang Dalam diusahakan oleh penduduk sebagai lahan pertanian. Namun hasil produksi pada daerah ini belum optimal yang disebabkan oleh belum baiknya jaringan tata air, dimana sebagian besar daerah tersebut merupakan daerah genangan, sering mengalami banjir pada musim penghujan serta mengalami kekeringan pada musim kemarau. Penelitian ini bertujuan untuk mengetahui jenis dan pengaruh hidrotopografi lahan terhadap saluran tersier, sehingga dapat diperoleh dimensi saluran tersier sesuai dengan peruntukan lahan di daerah rawa Pinang Dalam. Data primer pada penelitian ini yaitu data hidrometri dan data pasang surut, sementara data sekunder yang digunakan yaitu data hidrologi dan data topografi serta peta-peta yang diperlukan dalam analisis hidrotopografi. Data tersebut merupakan dasar dalam melakukan kajian dan analisis hidrometri dan topografi yang diperlukan untuk mengetahui hidrotopografi lahan dengan memperhatikan peruntukan lahan. Hasil penelitian menunjukkan bahwa jenis hidrotopografi lahan di daerah rawa Pinang Dalam terdiri dari jenis hidrotopografi B, C dan D. Berdasarkan jenis hidotopografi dan peruntukan lahan, terdapat kriteria tertentu mengenai kedalaman optimum untuk saluran tersier dalam sebuah jaringan tata air. Saluran tersier yang diperuntukkan sebagai lahan perkebunan sebaiknya diupayakan untuk memiliki kedalaman yang dapat mempertahankan muka air tanah dalam kisaran 60 hingga 90 centimeter, sementara elevasi muka air untuk tanaman padi sawah dipertahankan setinggi mungkin dengan kedalaman perakaran minus (-)10 sampai dengan -30 centimeter. [EN] The Pinang Dalam swamp area is a part of Pinang Komplek swamp area which is located in Kubu Raya Regency, West Kalimantan Province. Groundwater table in Pinang Dalam swamp area is affected by tides. Pinang Dalam area is cultivated by the population as agricultural land. But the production results in this area are not optimal due to the lack of a good water system, where most of the area is inundated, often experiences floods during the rainy season and experiences drought in the dry season. This research aims to identify the type and effects of land hydrotopography on the tertiary channel, thus the dimension of tertiary channel that is suitable for the allocated land use is obtained. The primary data in this study are hydrometric and tidal data, while secondary data used are hydrological and topographic data and maps needed in hydrotopographic analysis. These data are the basis for conducting studies and analysis of hydrometry and topography needed to the hydrotopography of land while taking the land use into account. The results showed that the hydrotopographic type of land in the Pinang Dalam swamp area consisted of hydrotopographic types B, C and D. Based on the hydotopography type and land use, there are certain criteria regarding the optimum depth for tertiary channels in a water system. Tertiary canals on land allocated as plantation area should be striven to have a depth that can maintain water table in the range of 60 to 90 centimeters, while the water level elevation for lowland rice plants should be maintained as high as possible with a rooting depth of minus (-) 10 to -30 centimeters.

scholarly journals SEDIMENT CARBON STOCK OF WEST KALIMANTAN MANGROVE FORESTS

2019 ◽  
Vol 44 (1) ◽  
pp. 27-35
Author(s):  
Tia Nuraya ◽  
Alan Frendy Koropitan ◽  
A'an Johan Wahyudi
Keyword(s):  
Organic Carbon ◽  
Carbon Stock ◽  
High Tide ◽  
Organic Carbon Content ◽  
Mangrove Forests ◽  
Dominant Type ◽  
West Kalimantan ◽  
Riverine Input ◽  
Sediment Carbon ◽  
Organic Carbon Stock

We investigate variation in sediment carbon stock at Mempawah and Bakau Besar in West Kalimantan by analyzing organic carbon content from sediment samples taken within 20 cm depth. Our results show that organic carbon stock of sediments in Bakau Besar is generally higher than in Mempawah that may be due to riverine input of organic carbon into the mangrove forests. The riverine input of organic carbon is influenced tides, in which we find that organic carbon loads are higher during high tide compared to low tide. In particular, we find high organic carbon contents at a station in Mempawah (Station 3; 6.46 ± 0.23 tons C/ha) and another station in Bakau Besar (Station 2; 14.93 ± 1.43 tons C/ha). These two stations have mangrove density of 13,519 individuals/ha and 9,928 individuals/ha, respectively. We conclude that high organic carbon is influenced by riverine input as well as a high density of mangrove and the dominant type of mangrove vegetation at the sites.

scholarly journals CHARACTERISTICS OF BREAKING WAVES AND ANALYSIS OF SEDIMENT TRANSPORT IN TELUK KENDARI

2018 ◽  
Vol 9 (2) ◽  
pp. 585-596
Author(s):  
Koko Ondara ◽  
Semeidi Husrin
Keyword(s):  
Sediment Transport ◽  
Wind Direction ◽  
High Tide ◽  
Distribution Patterns ◽  
Breaking Waves ◽  
Hydrodynamic Conditions ◽  
Wave Characteristics ◽  
Bay Area ◽  
Tidal Data ◽  
Wave Hindcasting

One of the problems that often occured in the bay area is a sedimentation process that occurred continuously, causing silting. The movement of sediment material in the process of sedimentation is influenced by the movement of the water flow like the tides, winds, currents and waves. The aim of this study was to determine the characteristics of the hydrodynamic conditions, particularly the distribution pattern and the capacity of the sediments in the Kendari Bay with oceanographic modeling approach. Bathymetry data measured at the site of the research conducted in August 2015. The analysis of distribution patterns of sedimentation, sedimentation capacity, wave hindcasting, wind data and tidal data using software, hindcasting results indicate the dominant wind direction coming from the east. Type tides in Kendari Bay is a mixed mainly semiurdunal tides. The concentration of suspended sediment at low tide is greater than at high tide.  Keywords: sediment transport, wave characteristics, Kendari Bay, hydro - dynamics, mike21

3. Measurement and prediction

2019 ◽  
pp. 34-49
Author(s):  
David George Bowers ◽  
Emyr Martyn Roberts
Keyword(s):  
Harmonic Analysis ◽  
Standard Method ◽  
Curve Fitting ◽  
Great Accuracy ◽  
Horizontal Flow ◽  
Physical Oceanography ◽  
Success Story ◽  
Fitting Procedure ◽  
Tidal Data ◽  
Tidal Streams

‘Measurement and prediction’ outlines the ways in which tides and tidal currents can be measured, and considers the standard method of analysing tidal data using a curve-fitting procedure known as harmonic analysis. Tides, unusually for natural events, can be forecast with great accuracy for years in advance. The ability to do this and make people safer at sea is probably the greatest practical success story of the science of physical oceanography. There are two aspects of the problem to be considered: the rise and fall of the level of the sea, which we shall call the tide; and the horizontal flow of the water, called tidal streams or currents.

Use of artificial collectors shows semilunar rhythm of planktonic dispersal in juvenile Hydrobia ulvae (Gastropoda: Prosobranchia)

2004 ◽  
Vol 84 (4) ◽  
pp. 761-766 ◽  
Author(s):  
Sónia Meireles ◽  
Henrique Queiroga
Keyword(s):  
Current Velocity ◽  
Cross Correlation ◽  
Tidal Range ◽  
Tidal Amplitude ◽  
Minimum Threshold ◽  
Hydrobia Ulvae ◽  
Cross Correlation Analysis ◽  
Average Current ◽  
Inexpensive Technique ◽  
Period Of Oscillation

The pattern of planktonic abundance of juvenile Hydrobia ulvae was investigated in the Ria de Aveiro, Portugal, with the use of floating artificial collectors made of ‘hoghair’ filter, which were deployed for 2-day consecutive periods during 3·5 months. Abundance in the collectors followed a remarkably regular semilunar pattern, being higher during spring tides around full and new moons. Cross-correlation analysis between tidal range and captures in the collectors indicated a period of oscillation of the captures of 15 d, with maximum captures tending to occur on the day of the highest amplitude tides. The physical and behavioural mechanisms responsible for the pattern remain largely unknown. However, results from a simple model assuming that migration from the sediment to the water is dependent on current velocity suggest there is a minimum threshold in average current velocity integrated along the tidal cycle (and, therefore, in tidal amplitude) above which juvenile H. ulvae exhibit the floating behaviour. Artificial collectors may provide an effective and relatively easy and inexpensive technique for the study of dispersal of post-metamorphic molluscs.

scholarly journals BIOGENIC GAS IN DELTAIC DEPOSITION ENVIRONMENT IN KAPUAS RIVER, WEST KALIMANTAN AND ITS UTILIZATIONS FOR LOCAL COMMUNITY

2016 ◽  
Vol 24 (2) ◽  
pp. 55
Author(s):  
Hananto Kurnio ◽  
Yudi Darlan
Keyword(s):  
Quartz Sand ◽  
Local Community ◽  
High Tide ◽  
Ground Surface ◽  
Gas Storage ◽  
West Kalimantan ◽  
Biogenic Gas ◽  
Below Ground ◽  
Fine Quartz ◽  
Gas Bubbling

Biogenic gas within a deltaic deposition environment in the Kapuas rivermouth of West Kalimantan occurred in fine to very fine quartz sand reservoir of shallow boreholes of having the depth of 1-12 m below ground surface. This reservoir is covered by peaty layers of semi-impermeable property. During high tide, gas bubbling took place in the water column above the ground of these semi-impermeable layers. Utilizations of biogenic gas had been done succesfully. These works were carried out through drilling, piping, gas storage and installations for gas stove and gas electricity generator of 500 watt capacity at chief village house as an example before widely used to the local community. Keywords: Biogenic Gas; Deltaic Deposition Environment; Kapuas River; west Kalimantan, Utilization. Gas biogenik dalam suatu lingkungan pengendapan delta di muara Sungai Kapuas Kalimantan Barat terdapat dalam reservoar pasir kuarsa berukuran halus hingga sangat halus pada kedalaman bor dangkal 1-12 m di bawah permukaan tanah. Reservoar ini ditutupi oleh lapisan gambut semiimpermeabel. Selama pasang naik, gelembung gas teramati dalam kolom air di atas permukaan lapisan semi-impermeabel ini. Pemanfaatan gas biogenik telah dilaksanakan dengan sukses. Pemanfaatan ini dilakukan melalui pemboran, pipanisasi, penampungan gas dan instalasi untuk kompor gas dan generator listrik berbahan bakar gas kapasitas 500 watt di rumah Kepala Desa sebagai contoh sebelum dimanfaatkan secara luas oleh masyarakat setempat. Kata kunci: Gas Biogenik, Lingkungan Pengendapan Delta, Sungai Kapuas, Kalimantan Barat, Pemanfaatan

scholarly journals Observing Surface Wave Directional Spectra under Typhoon Megi 2010 using Subsurface EM-APEX Floats

2021 ◽  
Author(s):  
Je-Yuan Hsu
Keyword(s):  
Surface Wave ◽  
Surface Waves ◽  
Current Velocity ◽  
Autonomous Vehicles ◽  
Wind Waves ◽  
Peak Frequency ◽  
Ocean Dynamics ◽  
Vertical Acceleration ◽  
Wave Direction ◽  
The Right

AbstractEM-APEX floats as autonomous vehicles have been used for profiling temperature, salinity and current velocity for more than a decade. In the traditional method for processing horizontal current velocity from float measurements, signals of surface wave motion are removed as residuals. Here, a new data processing method is proposed for deriving the horizontal velocity of surface waves at the floats. Combined with the vertical acceleration measurements of waves, surface wave directional spectra E(f,θ) can be computed. This method is applied to the float measurements on the right of Typhoon Megi’s track 2010. At 0.6 day before the passage of Megi’s eye to the floats, the fast-propagating swell may affect wind waves forced by the local storm wind. When the storm moves closer to the floats, the increasing wind speed and decreasing angle between wind and dominant wave direction may enhance the wind forcing and form a mono-modal spectrum E(f). The peak frequency fp ~ 0.08 Hz and significant wave height > 10 m are found near the eyewall. After the passage of the eye to the floats, the fp increases to > 0.1 Hz. Although E(f) still has a single spectral peak at the rear-right quadrant of Megi, E(f,θ) at frequencies from 0.08 to 0.12 Hz has waves propagating in three different directions as a tri-modal spectrum, partially due to the swell propagating from the rear-left quadrant. Enhancing the capability of EM-APEX floats to observe wave spectra is critical for exploring the roles of surface waves in the upper ocean dynamics in the future.

Sign in / Sign up

Export Citation Format

Share Document