Oil spill trajectory modelling of Chennai coast, east coast of India

Size: px
Start display at page:

Download "Oil spill trajectory modelling of Chennai coast, east coast of India"

Transcription

1 INCHOE (Proceedings) 5-7 Feb. Goa, India 9-99 Oil spill trajectory modelling of Chennai coast, east coast of India R. Mohan* 1, R.S. Kankara and R. Venkatachalapathy 3 1 -Department of Physics, Annamalai University, Annamalai Nagar-. Tamil Nadu, India. rethinamohan@gmail.com - Scientist-F, Ministry of Earth Sciences, ICMAM-PD, NIOT Campus, Pallikaranai, Chennai-, Tamil Nadu, India. kankara@icmam.gov.in 3 - Professor, Faculty of Marine Sciences, CAS-MB, Annamalai University, Parangipettai- 5, Tamil Nadu, India. venkatr5@rediffmail.com ABSTRACT Mohan, R., Kankara, R.S. and Venkatachalapathy, D.,. Oil spill trajectory modelling of Chennai coast, east coast of India, Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE), 5-7 Feb., CSIR-NIO, Goa, India. Computational modeling play a vital role in order to prepare the impact of an oil spill and preparedness for contingency plan. Oil spill trajectory modeling attempt was made at Chennai coast. The Chennai coast is one of the high risks area for oil spill due to its exposure to oil related activities i.e. oil refinery, sub-sea pipeline, port and harbor, economical importance and close to tanker routes. Number of ships/tankers is being handled at Chennai port. These have increased the risk of oil spill in the coastal waters. Numerical model was setup to investigate the potential risk of an accidental oil spill along Chennai coast. The two probable spill scenarios, one for Fuel oil leak ( m 3 ) for hours at off Marina and other for 5 m 3 of crude (Bombay High) oil for instantaneous spill at anchorage area (off port) were considered. Current and wind are two main factor for oil transport. Therefore, a hydrodynamic model was setup and calibrated using measured water level and current data. The calibrated model was used to generate the circulation pattern over the year required for generating monthly oil spill trajectory. The oil spill was simulated for hours duration for each month/season considering prevailing current and monthly mean wind condition. The model simulation revealed that the spilled oil had tendency to move towards south-west direction to reach sandy shore less than hours after the spill was occurred in the ocean during NE monsoon. The results for both leak and instantaneous spill indicate that spilled oil will not move towards the marina beach during SW monsoon. More than % of the diesel and 5% of crude oil will be evaporated within h of oil spill. Based on the results, a suitable cleanup and contingency plan can be devised to mitigate the adverse impacts arising due to diesel spill in the study area. ADDITIONAL INDEX WORDS: Numerical Model; diesel and crude oil spill; MIKE; Chennai coast. INTRODUCTION The main source of oil pollution in oceans is from shipping and maritime activities. Nearly half of the world production of oil has been transported by the sea route(clark, 199). More than three million metric tons of oil contaminates the sea every year. Operational or accidental release of oil into the sea has caused harmful effects on marine environment and marine life, making oil spills a matter of international concern and global issue. Indian coastline extends to about 5 kms on the mainland and to about kms along two groups of islands. The Arabian Sea and the Bay of Bengal have been estimated to annually receive around 5x and x t/y petroleum respectively from routine discharges from oil tankers and other ships (Hinrichsen, 9). The majority of ships sailing from the Persian Gulf to Japan and China transports oil through the Indian Exclusive Economic Zone (EEZ). The port sector handles a large volume of oil, and many numbers of new oil industries are being set up in the coastal zone. Seagoing transport of oil poses the risk of oil spills that may occur due to accidents, grounding of ships, tankers, etc., which would cause extensive damage to the marine ecosystem and the living resources. Since the preventive measures can not eliminate the risk of oil spills in marine waters, it is necessary for effective and suitable mitigating measures to know about the fate of an oil spill on marine water and its impact on the marine resources. The numerical modeling approach has emerged as a useful tool to simulate the scenarios and address the issue of oil dispersion in the case of a spill. Computer models provide a valuable support to make predictions about the trajectory and fate of spilled oil in marine environment. Several oil spill models have been used in the past three decades based on transport and weathering processes (Kankara and Subramanian, 7; Kolluru et al., 199; Mackay et al., 19; Naidu et al., 13; Tkalich et al., 3; Vethamony et al., 7) In the present study, an attempt has been made to investigate the potential risk of an accidental oil spill along Chennai coast. STUDY AREA The Chennai coast is one of the high risk areas for oil spill due to its exposure to oil related activities i.e. oil refinery, subsea pipeline, port and harbour, economical importance and close to tanker routes. Number of ships/tankers is being handled at Chennai port. These have increased the risk of oil spill in the coastal waters. The past two decades, four oil spills incidents are reported in Chennai coastal water i.e. during August 199, November 199 and 1995 and January (Bluewaters., ). It shows the potential risks of oil spills Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 9

2 Oil spill trajectory modelling along Chennai coast. A major spill may occur during normal operations, illegal oil releases like bilge water releases, tank washing, etc. These are created oil pollution threatens for coastal environment, tourist beaches and affect unfavorably the economic, ecological and biological life. The shortest time for the oil to reach the shoreline was identified through the numerical model simulation of the trajectory model as well as to estimate weathering process under the specified hydrodynamic and meteorological conditions. The study area is located between the longitudes of E and E and the latitudes of 5 N and N coast of 3 km long coastal stretch from Tiruvottiyur to Neelankarai. The coastal stretch containing fishing harbour, Chennai port, Adyar and Coovum river mouth, Marina & Besant nagar beach, Astalakshmi temple, Santhome church are located along the coast in study area (Figure 1). The coastline orientation is about in Northern part and in Southern side (Kankara et al., 11). Figure 1. Chennai coastal region MATERIAL AND METHODS A numerical modeling technique is applied for simulating spatial and temporal patterns of an oil spill under given environmental conditions. The numerical modeling approach has been emerged as a useful tool to simulate various scenarios of likely oil spills to understand the fate and behavior of oil for given scenerio. Two modelling packages i.e. MIKE-1 and ADIOS were used to simulate the oil spill in Chennai coast. MIKE-1 was used to generate the oil trajectory and to track the path of spilled oil under prevailing hydrodynamic and meteorological conditions. The two modules, namely MIKE1-HD for generating the hydrodynamics and Spill Analysis (SA) for spreading and dispersion analysis of hydrocarbons in marine environments, were used. The oil spill module MIKE 1 (SA) applies a Lagrangian discrete parcel method to predict the trajectory of spilled oil and estimate the fate and behavior of oil spills based on complex algorithmsdhi. (7). In the model, the oil is represented by a large ensemble of marked particles. The movement of each particle is affected by the Physio-chemical processes. Once the parcels are released in the water body, their discrete path and mass are followed and recorded as a function of time relative to the reference grid system. The details of depth-averaged two-dimensional hydrodynamic model are described Kankara et al. (11), were used to link oil spill module and to provide the data for the water movement in the study area. The weathering model ADIOS (Automated Data Inquiry for Oil Spills) predicts the changes in oil characteristics that may occur over time, under the influence of a variety of environmental conditions. ADIOS uses mathematical equations and information from the database to predict changes over time in the density, viscosity and water content of an oil or product, the rates at which it evaporates from the sea surface and disperses into the water, and the rate at which an oil-inwater emulsion may be formed Lehr et al. (1997). It was designed to make use of as little information as possible, and to use information that can quickly be estimated or obtained in the field, such as wind speeds, wave heights, water temperature, and salinity or density, the type and amount of oil or product spilled, and the rate and duration of the spill Lehr et al. (). Accordingly different oil spill scenarios were considered at specific period and trajectories of oil spill were studied for two different locations along Chennai coast. The fundamental of actual spill scenario with the information of oil type, volume of spill, release duration and release location, climatic condition are tabulated (Table 1). A hypothetical accidental spill of diesel and crude oil was used in this study. The results of the trajectory and fate model calculation determine both travel times and location of shoreline oiling, together with slick volume and amounts evaporated, dispersed and emulsified over time. Table 1. Details of scenarios considered in present study. Spill site with coordinates off Marina beach (.31917, 13.) Off Chennai port (.9, ) Channel ( , ) Spill duration *Predominant Mean Wind Effect Water depth (m) Type of oil Diesel Fuel Oil Spill volume (m 3 ) Crude Oil 5 hours Heavy Fuel Oil SW monsoon NE monsoon (I) Hydrodynamic simulation Climatic Scenarios SW and NE monsoon SW and NE monsoon Spill type Continuous Instantaneous 5 Monthly Instantaneous Wind Consideration Predominant Mean Wind speed and Wind direction * Predominant Mean Wind speed and Wind direction * Monthly Wind speed and Wind direction Wind Speed =. m/s: Wind Direction = 33 degree Wind Speed =. m/s: Wind Direction = 7 degree RESULTS The simulations of hydrodynamic model was calibrated and validated with the observed data and was used in the oil spill simulations. A typical plot of water surface elevation, current Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 95

3 Mohan et al. speed and direction during NE monsoon condition are shown in figure. The length of the arrows shows the current direction and speed in the region. It was observed that the flow is towards southern direction. The model computed surface elevation are well comparable with field data and are grossly comparable for U and V velocity components to the overall period. The model computed surface elevation and V velocity component are highly correlated with observed data for.9 and.7 and moderate for U component (.1). The relative mean absolute error (RMAE) and index of agreement (IoAd) was. and.9 for surface elevation and.7 and.7 for U component and. and.5 for V component Kankara et al. (11). This hydrodynamic model along with monthly mean wind data was used to simulate monthly oil spill scenarios which are very useful for contingency plan. (II) Oil spill Simulations (a) Scenario-I (Oil spill at off Marina beach) In this case, the source location of spilled oil was selected off Marina beach over the duration of hours, m 3 of diesel fuel oil of accidential spill (continuous) at a depth of m. The predominant mean wind speed of. and. m/s and mean wind direction of 3 and 7 during SW and NE monsoon respectively were taken to run the model. During SW monsoon, the direction of spilled oil movement was noticed parallel to the shore towards north-north-east direction. The movement of the oil slicks and flow direction on the water surface was influenced by uni-directional coastal current and wind. During SW monsoon, spilled oil does not reach the coast. The oil in the water column runs up to hours from the time of initial spill and pass away from the model domain during SW monsoon (Figure 3a). Similarly, during NE monsoon, the slick movement was noticed towards the southwest direction (Figure 3b). The spilled oil reaches the shore within 3 hours after the spill and may affect the coastal reagion of marina beach. The. cm size of oil slick affected the shore and and migrated around a length of 1 km. (b) Scenario-II (Oil spill at anchorage area (off port)) The effect of wind force on the instantaneous spilled oil concentration on the surface area is examined. The oil spill simulation was carried out for hours, with a volume of 5 m 3 for crude oil at a depth of m along the specified spill site (anchorage area (off port)). The model was run to predict the movement of oil in both SW and NE season with predominant mean wind effect like scenario-i. The movement of oil spill was monitored after hours from the initial time. It was found that, the oil spill was moving towards north-north-east and south-south-west direction during SW and NE monsoon season respectively (Figure a&b). During the SW monsoon, the spilled oil crosses away from the model domain whereas, the oil dispersed in the water column over a period of time in NE monsoon. From the results it was found that there is no impact in the near-shore region, which may be due to the direction of tidal current and occurance of oil spill away from the coast. Figure. Synoptic view of current vector plot for NE monsoon 1 a) b) /11/ :: Scale 1: 1// :: Scale 1:1139 Figure 3. Simulated trajectory of diesel oil spill at off Marina with predominant wind effects during a) SW and b) NE monsoon Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 9

4 Oil spill trajectory modelling 1 a) b) WS= m/s 1 WD=5 WD=7 WD=7 July August September WS=3 m/s 1 WD=5 WD= WD= // 1:: Scale 1:1139 1/5/ 1:: Scale 1:1139 Figure. Simulated trajectory of instantaneous spilled oil at anchorage area (off port) with predominant wind effects during a) SW and b) NE monsoon. October November December Figure. Monthly scenarios of spill for the duration of every hours during July to December. (c) Scenario-III (Simulation of monthly oil spill thickness and trajectories of hypothetical spill location of shipping channel) The effect of the monthly mean wind force at the instantaneously spilled oil concentration on the surface area is examined. For a specified spill site (shipping channel), the simulation was carried out for hours of the oil spill and observation was made for every hours about the volume of 5 m 3 for heavy fuel oil. The model has been run for predicting the total concentration of oil spilled with the varying wind speed and direction. After hours from beginning, the release of spilled oil was monitored. It was found that the oil spill reached the shore for the wind direction of E and SE. Chennai port and Royapuram fishing harbor areas are affected by this movement of spill during February, March, April and May. The movement of spilled oil was noticed towards SW direction during the month of October, November, December and January and may affect Marina beach and Coovum. From June to September, spill movement was observed towards NNE direction and oil found floating in water column. 1 1 WD=5 WS=.5 m/s WD=135 WD=9 WS=.5 m/s WD=135 WS= m/s WD=135 January February March WS=.5 m/s WD=7 The movement of the spilled oil particle was found which is due to uni-directional tidal current flow with the influence of wind also. The overall simulation results reveal that the surface oil thickness varied between and. cm (Figure 5 and ). These studies provids very valuable information of actual situation of an oil spill at the Chennai coast. (III) Simulation of Weathering Process As a second stage of simulation, the weathering conditions were analysed using ADIOS. The model has been run for the SW monsoon environmental conditions such as water temperature ( C), wind speed (. m/s), wind direction (3 ), current speed and direction (. m/s & ), wave height (. m) and salinity (3 ppt). Preplanning for a selection of oil can provide an excellent guidance during a weathering process and the m 3 volume of oil was selected from the model database. The oil mass balance was computed for Fuel oil no. (Diesel) and evaporation, vertical dispersion is simulated to yield estimates of the total volume of oil remaining. It was found that the model over forecasts about leaked oil for 15-% was lost due to evaporation during the early hours and -5% was vertically dispersed in the water column within 15 hours out of hours of duration (Figure 7). From the Figure, the model has been run for the NE monsoon environmental conditions such as water temperature ( C), wind speed (. m/s), wind direction (7 ), current speed and direction (. m/s & ), wave height (. m) and salinity (3 ppt). The 5 m 3 volumes of crude oil were selected from the model database. The simulation result reveals that % was lost due to evaporation during the early hours and 7-% was vertically dispersed in the water column more than hours of duration. April May June Figure 5. Monthly scenarios of spill for the duration of every hours during January to June. Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 97

5 Oil viscosity (cst) Mohan et al. Figure 9 show the change in oil viscosity. As can be see, the viscosity of oil changes significantly with evaporation. If about % oil evaporates, their viscosities increase more than and times for diesel and crude oil respectively. DISCUSSION Figure 7. The fate of m 3 volume of diesel fuel oil leakage Figure. The fate of 5 m 3 volumes of instantaneous crude oil spill 1 Jun 7 Jun Jun 9 Jun a) Jun 11 The overall simulation results reveal that the surface oil concentration was varied between.5 and.3 cm for diesel fuel oil whereas, 5 and cm for crude oil. The movement of the spilled oil particle was found which is due to unidirectional tidal current flow with also the wind. From the findings, during SW monsoon the spilled oil at off Marina not reaching the shoreline does not mean that it will not pollute the water. The minimal impact was found along the shoreline for oil spilled at off Marina beach which may affect biological activities at near-shore region during SW monsoon. During NE monsoon, the oil patches reaches the shoreline and impacts were found to be high on Marina beach. Generally, the impact of spill is high along Marina beach which is nearest to Chennai port. The movement of spilled oil off port was noticed towards south-south-west direction during SW monsoon whereas, north-north-east during NE monsoon season. There is no impact in near-shore region and oil in the water column. However, the oil dispersion in the water column increased considerably with time due to the increase in density of oil and the variation of viscosity. The shoreline of Chennai and their area of operation are very sensitive due to the sandy beach, port activities, settlements, etc. The highest percentage of evaporation and lowest dispersion were noticed in the diesel oil due to its low viscosity. The results shows that the evaporation process was very fast at the initial stage of spill and slowed down subsequently. The results revealed that the priorities should be given to protect the area due to spilled oil along the Chennai coast as Marina beach, Chennai port, Fishing harbor, Coovum and Adyar river mouth, Elliot beach. These studies provides very valuable information for the consideration of the actual situation of an oil spill at the Chennai coast. If the spill occurred in this region, it may affect not only in terms of human life and the environment but also for coastal economies. This analysis provides valuable information that the oil remediation using dispersant or application of booms will be effective in the initial phase of spill. The residual oil, along with dispersed and dissolved components, would be a threat to a coastal and marine environment because either it would hit the coast or disperse in the water column over a period of time. Analysis of the oil transport, weathering, and computed oil thickness provides a way to investigate the environmental risks to the marine ecosystem due to a spill. 1 Jan Jan 5 Jan Jan 7 b) Jan Figure 9. The change in oil viscosity of a) Diesel and b) Crude oil CONCLUSIONS The monthly simulation of a hypothetical accidental oil spill showed that, the movements of oil mainly rely on the combined effect of tidal current and wind. In SW monsoon, the spill moves towards north-north-east direction while it moves south-south-west during NE monsoon. During NE monsoon season, the spilled oil has prolonged contact shoreline. The results shows that the spill occurred in nearshore region will reach the shoreline within to 3 hours depending on wind speed and direction. The oil mass balance was computed with hours of simulation for diesel and crude oil with their different volume. It was found that % of diesel oil was lost due to evaporation and -5% was vertically dispersed in the water column within 15 hours out of hours Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 9

6 Oil spill trajectory modelling of duration. The % crude oil was evaporated and 7-% was dispersed in water column. The results are useful for both industry and government agencies, which require specific information at the planning stage or to respond to a spill incident. ACKNOWLEDGMENTS Tkalich, P., Huda, K. and Hoong Gin, K.Y., 3. A multiphase oil spill model. Journal of Hydraulic Research, 1(): Vethamony, P. et al., 7. Trajectory of an oil spill off goa, eastern arabian sea: Field observations and simulations. Environmental Pollution, (): 3-. The authors wish to express their sincere thanks to Dr. Sailesh R. Nayak, Secretary, Ministry of Earth Sciences, and Dr.M. Atmanand, Director, ICMAM-PD, Chennai and Dr. B.R. Subramanian, Former Director, ICMAM-Project Directorate, for their constant encouragement and for providing the requisite facilities for carrying out this work. The authors gratefully acknowledge Dr. T. Balasubramanian, Former Director, Faculty of Marine Science, Centre of Advanced Study in Marine Biology, Annamalai University, Parangipettai, and his team for their valuable support during the field campaign. REFERENCES Bluewaters.,. Blue waters : Newsletter on marine environment security. Blue waters : newsletter on marine environment security. Clark, R.B., 199. Marine pollution. Oxford University Press, New York. DHI., 7. Scientific documentation, mike 1 oil spill module, dhi water and environment. Horsholm, denmark: Dhi software. Hinrichsen, D., 9. Our common seas : Coasts in crisis / don hinrichsen. [electronic resource]. Sterling, VA Earthscan, International Institute for Environment and Development. Kankara, R.S., Mohan, R. and Venkatachalapathy, R., 11. Hydrodynamic modelling of chennai coast from a coastal zone management perspective. Journal of Coastal Research: Kankara, R.S. and Subramanian, B.R., 7. Oil spill sensitivity analysis and risk assessment for gulf of kachchh, india, using integrated modeling. Journal of Coastal Research: Kolluru, V., Spaulding, M.L. and Anderson, E., 199. A three dimensional subsurface oil dispersion model using a particle based approach. ARCTIC AND MARINE OILSPILL PROGRAM TECHNICAL SEMINAR, p.^pp.. Lehr, W., Jones, R., Evans, M., Simecek-Beatty, D. and Overstreet, R.,. Revisions of the adios oil spill model. Environmental Modelling and Software with Environment Data News, 17(): Lehr, W., Overstreet, R., Jones, R., Eclipse, L. and Simecek- Beatty, D., The next generation in oil weathering modeling. International Oil Spill Conference Proceedings, 1997(1): Mackay, D., Paterson, S. and Trudel, K., 19. Mathematical model of oil spill behavior. Environment Canada. Naidu, V.S., Sukumaran, S., Dubbewar, O. and Reddy, G.S., 13. Operational forecast of oil spill trajectory and assessment of impacts on intertidal macrobenthos in the dahanu region, west coast of india. Journal of Coastal Research: Proceedings of the Fifth Indian National Conference on Harbour and Ocean Engineering (INCHOE) 99

Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy

Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy Computational Analysis of Oil Spill in Shallow Water due to Wave and Tidal Motion Madhu Agrawal Durai Dakshinamoorthy 1 OUTLINE Overview of Oil Spill & its Impact Technical Challenges for Modeling Review

More information

Currents measurements in the coast of Montevideo, Uruguay

Currents measurements in the coast of Montevideo, Uruguay Currents measurements in the coast of Montevideo, Uruguay M. Fossati, D. Bellón, E. Lorenzo & I. Piedra-Cueva Fluid Mechanics and Environmental Engineering Institute (IMFIA), School of Engineering, Research

More information

Presented by. Mr.Danish.D.R. M.Tech Coastal Management Institute for Ocean Management Anna University, Chennai Tamil Nadu, India.

Presented by. Mr.Danish.D.R. M.Tech Coastal Management Institute for Ocean Management Anna University, Chennai Tamil Nadu, India. MATHEMATICAL MODEL STUDY OF THE EFFLUENT DISPOSAL FROM A DESALINATION PLANT IN THE MARINE ENVIRONMENT AT TUTICORIN Presented by Mr.Danish.D.R M.Tech Coastal Management Institute for Ocean Management Anna

More information

Training program on Modelling: A Case study Hydro-dynamic Model of Zanzibar channel

Training program on Modelling: A Case study Hydro-dynamic Model of Zanzibar channel Training program on Modelling: A Case study Hydro-dynamic Model of Zanzibar channel Mayorga-Adame,C.G., Sanga,I.P.L., Majuto, C., Makame, M.A., Garu,M. INTRODUCTION Hydrodynamic Modeling In understanding

More information

Testing of a oil spill mathematical model contained in PISCES II simulator

Testing of a oil spill mathematical model contained in PISCES II simulator Scientific Journals Maritime University of Szczecin Zeszyty Naukowe Akademia Morska w Szczecinie 212, 32(14) z. 2 pp. 15 19 212, 32(14) z. 2 s. 15 19 Testing of a oil spill mathematical model contained

More information

Available online at ScienceDirect. Procedia Engineering 116 (2015 )

Available online at  ScienceDirect. Procedia Engineering 116 (2015 ) Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 116 (2015 ) 320 325 8th International Conference on Asian and Pacific Coasts (APAC 2015) Department of Ocean Engineering, IIT

More information

Wave Energy Atlas in Vietnam

Wave Energy Atlas in Vietnam Wave Energy Atlas in Vietnam Nguyen Manh Hung, Duong Cong Dien 1 1 Institute of Mechanics, 264 Doi Can Str. Hanoi, Vietnam nmhungim@gmail.com; duongdienim@gmail.com Abstract Vietnam has achieved remarkable

More information

An independent study to assess and validate the shape and size of the Potentially Impacted Areas used in BEAWARE 2 Qualitative results

An independent study to assess and validate the shape and size of the Potentially Impacted Areas used in BEAWARE 2 Qualitative results An independent study to assess and validate the shape and size of the Potentially Impacted Areas used in BEAWARE 2 Qualitative results Project: BE-AWARE II Author : Sébastien Legrand Reference: MFC/2015/SL/BE-AWARE/report_potentially_impacted_areas_v1.1

More information

HYDROSPHERE, OCEANS AND TIDES

HYDROSPHERE, OCEANS AND TIDES HYDROSPHERE, OCEANS AND TIDES Revision 10x10learning.com 1 Chapter 12. In the Earth s Atmosphere On surface of the Earth Under the ground Hydrosphere comprises of ALL WATER Water Vapour = 0.001% Is very

More information

Case Studies. Georg Umgiesser and Natalja Čerkasova KU, Lithuania

Case Studies. Georg Umgiesser and Natalja Čerkasova KU, Lithuania Case Studies Georg Umgiesser and Natalja Čerkasova KU, Lithuania Case 1: A beach in the Curonian Lagoon Beach Current situation in Curonian lagoon Beach in Kintai In the past, especially in Baltic inner

More information

THE WAVE CLIMATE IN THE BELGIAN COASTAL ZONE

THE WAVE CLIMATE IN THE BELGIAN COASTAL ZONE THE WAVE CLIMATE IN THE BELGIAN COASTAL ZONE Toon Verwaest, Flanders Hydraulics Research, toon.verwaest@mow.vlaanderen.be Sarah Doorme, IMDC, sarah.doorme@imdc.be Kristof Verelst, Flanders Hydraulics Research,

More information

July Interim Report. National Institute of Wind Energy (NIWE) Wind Resource Assessment & Offshore Unit Chennai, India.

July Interim Report. National Institute of Wind Energy (NIWE) Wind Resource Assessment & Offshore Unit Chennai, India. Interim Report (First Offshore Lidar wind data analysis) July 2018 Prepared by National Institute of Wind Energy (NIWE) Wind Resource Assessment & Offshore Unit Chennai, India. W I N D R E S O U R C E

More information

PHYSICAL AND NUMERICAL MODELLING OF WAVE FIELD IN FRONT OF THE CONTAINER TERMINAL PEAR - PORT OF RIJEKA (ADRIATIC SEA)

PHYSICAL AND NUMERICAL MODELLING OF WAVE FIELD IN FRONT OF THE CONTAINER TERMINAL PEAR - PORT OF RIJEKA (ADRIATIC SEA) PHYSICAL AND NUMERICAL MODELLING OF WAVE FIELD IN FRONT OF THE CONTAINER TERMINAL PEAR - PORT OF RIJEKA (ADRIATIC SEA) DALIBOR CAREVIĆ (1), GORAN LONČAR (1), VLADIMIR ANDROČEC (1) & MARIN PALADIN (1) 1.

More information

Oil spill drift study for NORTHER By V. Dulière and S. Legrand

Oil spill drift study for NORTHER By V. Dulière and S. Legrand October 2011 Oil spill drift study for NORTHER By V. Dulière and S. Legrand 1. Introduction The risk for navigation accident and therefore also for oil spilled at sea increases with the installation of

More information

IMPACTS OF COASTAL PROTECTION STRATEGIES ON THE COASTS OF CRETE: NUMERICAL EXPERIMENTS

IMPACTS OF COASTAL PROTECTION STRATEGIES ON THE COASTS OF CRETE: NUMERICAL EXPERIMENTS IMPACTS OF COASTAL PROTECTION STRATEGIES ON THE COASTS OF CRETE: NUMERICAL EXPERIMENTS Tsanis, I.K., Saied, U.M., Valavanis V. Department of Environmental Engineering, Technical University of Crete, Chania,

More information

National Oil Spill Contingency Plan. Chapter 2 Forms

National Oil Spill Contingency Plan. Chapter 2 Forms National Oil Spill Contingency Plan Chapter 2 Forms Contents Overview... 3 Summary of Forms... 3 Pollution Incident Evaluation Form... 3 Notification of a Marine Oil Spill... 3 Offshore Installation Notification

More information

A numerical simulation of oil spill in Istanbul strait

A numerical simulation of oil spill in Istanbul strait Coastal Engineering 135 A numerical simulation of oil spill in Istanbul strait S. Can 1, S. Nishio 2 & M. Uchida 2 1 Maritime Faculty Istanbul Technical University, Turkey 2 Faculty of Maritime Sciences,

More information

Shoreline Evolution Due to Oblique Waves in Presence of Submerged Breakwaters. Nima Zakeri (Corresponding Author), Mojtaba Tajziehchi

Shoreline Evolution Due to Oblique Waves in Presence of Submerged Breakwaters. Nima Zakeri (Corresponding Author), Mojtaba Tajziehchi Shoreline Evolution Due to Oblique Waves in Presence of Submerged Breakwaters Nima Zakeri (Corresponding Author), Mojtaba Tajziehchi Department of Civil Engineering, Faculty of Engineering, University

More information

The ocean water is dynamic. Its physical

The ocean water is dynamic. Its physical CHAPTER MOVEMENTS OF OCEAN WATER The ocean water is dynamic. Its physical characteristics like temperature, salinity, density and the external forces like of the sun, moon and the winds influence the movement

More information

STUDY ON TSUNAMI PROPAGATION INTO RIVERS

STUDY ON TSUNAMI PROPAGATION INTO RIVERS ABSTRACT STUDY ON TSUNAMI PROPAGATION INTO RIVERS Min Roh 1, Xuan Tinh Nguyen 2, Hitoshi Tanaka 3 When tsunami wave propagation from the narrow river mouth, water surface is raised and fluctuated by long

More information

A process based approach to understand WA s complex coastline Jeff Hansen Ryan Lowe Graham Symonds Laura Segura Gundula Winter

A process based approach to understand WA s complex coastline Jeff Hansen Ryan Lowe Graham Symonds Laura Segura Gundula Winter A process based approach to understand WA s complex coastline Jeff Hansen Ryan Lowe Graham Symonds Laura Segura Gundula Winter WA s coastline is highly variable due to offshore and shore-attached coral

More information

Inlet Management Study for Pass-A-Grille and Bunces Pass, Pinellas County, Florida

Inlet Management Study for Pass-A-Grille and Bunces Pass, Pinellas County, Florida Inlet Management Study for Pass-A-Grille and Bunces Pass, Pinellas County, Florida Final Report Submitted By Ping Wang, Ph.D., Jun Cheng Ph.D., Zachary Westfall, and Mathieu Vallee Coastal Research Laboratory

More information

from a decade of CCD temperature data

from a decade of CCD temperature data (Some of) What we have learned from a decade of CCD temperature data Craig Gelpi and Karen Norris Long Beach Aquarium of the Pacific August 15, 2008 Introduction Catalina Conservancy Divers collected temperature

More information

Inter-comparison of wave measurement by accelerometer and GPS wave buoy in shallow water off Cuddalore, east coast of India

Inter-comparison of wave measurement by accelerometer and GPS wave buoy in shallow water off Cuddalore, east coast of India Indian Journal of Geo-Marine Sciences Vol. 43(1), January 2014, pp. 45-49 Inter-comparison of wave measurement by accelerometer and GPS wave buoy in shallow water off Cuddalore, east coast of India Sisir

More information

HELCOM Submerged and The Nairobi International Convention. HELCOM Submerged Expert Group meeting in Bonn, Germany, 22 nd of April 2015

HELCOM Submerged and The Nairobi International Convention. HELCOM Submerged Expert Group meeting in Bonn, Germany, 22 nd of April 2015 HELCOM Submerged and The Nairobi International Convention HELCOM Submerged Expert Group meeting in Bonn, Germany, 22 nd of April 2015 The Nairobi International Convention on the Removal of Wrecks 2007

More information

CHAPTER 6 DISCUSSION ON WAVE PREDICTION METHODS

CHAPTER 6 DISCUSSION ON WAVE PREDICTION METHODS CHAPTER 6 DISCUSSION ON WAVE PREDICTION METHODS A critical evaluation of the three wave prediction methods examined in this thesis is presented in this Chapter. The significant wave parameters, Hand T,

More information

EXPERIMENTAL STUDY ON THE HYDRODYNAMIC BEHAVIORS OF TWO CONCENTRIC CYLINDERS

EXPERIMENTAL STUDY ON THE HYDRODYNAMIC BEHAVIORS OF TWO CONCENTRIC CYLINDERS EXPERIMENTAL STUDY ON THE HYDRODYNAMIC BEHAVIORS OF TWO CONCENTRIC CYLINDERS *Jeong-Rok Kim 1), Hyeok-Jun Koh ), Won-Sun Ruy 3) and Il-Hyoung Cho ) 1), 3), ) Department of Ocean System Engineering, Jeju

More information

INDIA METEOROLOGICAL DEPARTMENT (MINISTRY OF EARTH SCIENCES) SOUTHWEST MONSOON-2010 END OF SEASON REPORT

INDIA METEOROLOGICAL DEPARTMENT (MINISTRY OF EARTH SCIENCES) SOUTHWEST MONSOON-2010 END OF SEASON REPORT INDIA METEOROLOGICAL DEPARTMENT (MINISTRY OF EARTH SCIENCES) SOUTHWEST MONSOON-2010 END OF SEASON REPORT HIGHLIGHTS For the country as a whole, the rainfall for the season (June-September) was 102% of

More information

Deep water plume models - What s special about deep water

Deep water plume models - What s special about deep water Deep water plume models - What s special about deep water Øistein Johansen Senior scientist SINTEF Marine Environmental Technology Deep water blowouts - knowledge basis Present knowledge based on General

More information

Shoreline changes and reef strengthening at Kavaratti island in Lakshadweep Archipelago - A case study

Shoreline changes and reef strengthening at Kavaratti island in Lakshadweep Archipelago - A case study Indian Journal of Geo-Marine Sciences Vol. 43(7), July 2014, pp. 1140-1144 Shoreline changes and reef strengthening at Kavaratti island in Lakshadweep Archipelago - A case study T.N.Prakash*, L.Sheela

More information

OFFSHORE WIND ENERGY POTENTIAL ALONG INDIAN COAST

OFFSHORE WIND ENERGY POTENTIAL ALONG INDIAN COAST International Journal of Civil Engineering and Technology (IJCIET) Volume 9, Issue 7, July 2018, pp. 1480 1486, Article ID: IJCIET_09_07_157 Available online at http://www.iaeme.com/ijciet/issues.asp?jtype=ijciet&vtype=9&itype=7

More information

Chapter. The Dynamic Ocean

Chapter. The Dynamic Ocean Chapter The Dynamic Ocean An ocean current is the mass of ocean water that flows from one place to another. 16.1 The Composition of Seawater Surface Circulation Surface Currents Surface currents are movements

More information

STUDIES ON THE TRANQUILITY INSIDE THE GOPALPUR PORT

STUDIES ON THE TRANQUILITY INSIDE THE GOPALPUR PORT STUDIES ON THE TRANQUILITY INSIDE THE GOPALPUR PORT INTRODUCTION Sundar. V 1, Sannasiraj. S. A 2 and John Ashlin. S 3 Gopalpur port is an artificial harbor located in Odisha state. The geographical location

More information

SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011

SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011 SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011 1. At 20 N, both the ocean and the atmosphere carry approximately 2 PW of heat poleward, for a total of about 4 PW (see figure). If (at this latitude)

More information

Simulation of hydraulic regime and sediment transport in the Mekong delta coast

Simulation of hydraulic regime and sediment transport in the Mekong delta coast Simulation of hydraulic regime and sediment transport in the Mekong delta coast 1. Introduction Coastal erosion in the Mekong Delta has been recorded in recent years and the erosion rate has been increasing

More information

Journal of Applied Fluid Transients, Vol 1-1, April 2014 (3-1)

Journal of Applied Fluid Transients, Vol 1-1, April 2014 (3-1) Modeling and Field Verification Study of Air Slam Conditions on kalanit Pipeline System By Yiftach Brunner & Sathish Kumar ir valves are integral part of long water transmission mains and are essential

More information

Case Studies Georg Umgiesser and Natalja Čerkasova KU, Lithuania

Case Studies Georg Umgiesser and Natalja Čerkasova KU, Lithuania Case Studies Georg Umgiesser and Natalja Čerkasova KU, Lithuania Case 1: A beach in the Curonian Lagoon 1 Beach Current situation in Curonian lagoon Beach in Kintai In the past, especially in Baltic inner

More information

Study of Passing Ship Effects along a Bank by Delft3D-FLOW and XBeach1

Study of Passing Ship Effects along a Bank by Delft3D-FLOW and XBeach1 Study of Passing Ship Effects along a Bank by Delft3D-FLOW and XBeach1 Minggui Zhou 1, Dano Roelvink 2,4, Henk Verheij 3,4 and Han Ligteringen 2,3 1 School of Naval Architecture, Ocean and Civil Engineering,

More information

Section 6. The Surface Circulation of the Ocean. What Do You See? Think About It. Investigate. Learning Outcomes

Section 6. The Surface Circulation of the Ocean. What Do You See? Think About It. Investigate. Learning Outcomes Chapter 5 Winds, Oceans, Weather, and Climate Section 6 The Surface Circulation of the Ocean What Do You See? Learning Outcomes In this section, you will Understand the general paths of surface ocean currents.

More information

The Various Components of the Circulation in the Singapore Strait Region: Tidal, Wind and Eddy-driven Circulations and Their Relative Importance

The Various Components of the Circulation in the Singapore Strait Region: Tidal, Wind and Eddy-driven Circulations and Their Relative Importance The Various Components of the Circulation in the Singapore Strait Region: Tidal, Wind and Eddy-driven Circulations and Their Relative Importance Haoliang Chen CENSAM, Singapore-MIT Alliance for Research

More information

consulting engineers and scientists

consulting engineers and scientists consulting engineers and scientists Coastal Processes Presented by: January 9, 2015 Varoujan Hagopian, P.E. F.ASCE Senior Consultant, Waterfront Engineer Living Shoreline Workshop Lets Remember Why We

More information

COASTAL MORPHODYNAMICS

COASTAL MORPHODYNAMICS COASTAL MORPHODYNAMICS PATRICIA CHARDÓN-MALDONADO, PHD, EIT Miguel Canals, Jack A. Puleo, Alec Torres-Freyermuth & Jens Figlus March 9, 2017 OUTLINE INTRODUCTION Meteorological Phenomena Forcing Conditions

More information

OPERATIONS SEAFARER CERTIFICATION GUIDANCE NOTE SA MARITIME QUALIFICATIONS CODE. Deck: Chart Work

OPERATIONS SEAFARER CERTIFICATION GUIDANCE NOTE SA MARITIME QUALIFICATIONS CODE. Deck: Chart Work Page 1 of 6 Compiled by Approved by Chief Examiner Syllabus Committee: 26 February 2013 OPERATIONS SEAFARER CERTIFICATION GUIDANCE NOTE SA MARITIME QUALIFICATIONS CODE Deck: Chart Work Page 2 of 6 COLUMN

More information

Available online at ScienceDirect. Procedia Engineering 116 (2015 )

Available online at  ScienceDirect. Procedia Engineering 116 (2015 ) Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 116 (2015 ) 398 405 8th International Conference on Asian and Pacific Coasts (APAC 2015) Department of Ocean Engineering, IIT

More information

Deep Water Currents Lab

Deep Water Currents Lab Deep Water Currents Lab Background: Anyone visiting the seashore is struck by the constant motion of water traveling on the surface of the ocean in the form of waves. But beneath the ocean's surface, water

More information

Chapter 22, Section 1 - Ocean Currents. Section Objectives

Chapter 22, Section 1 - Ocean Currents. Section Objectives Chapter 22, Section 1 - Ocean Currents Section Objectives Intro Surface Currents Factors Affecting Ocean Currents Global Wind Belts (you should draw and label a diagram of the global wind belts) The Coriolis

More information

Mechanisms and Characteristics of High-Speed Reef Rip Current

Mechanisms and Characteristics of High-Speed Reef Rip Current Mechanisms and Characteristics of High-Speed Reef Rip Current Ryuichiro Nishi, Mario P. de Leon, Kouji Horinouchi,Akira Ohtani, Nicholas C. Kraus, and Julianti K. Manu Many people utilize beaches, but

More information

Feasibility Study for Dredging of Khaprabhanga Chapalir Don River in Patuakhali District for Improvement of Navigability

Feasibility Study for Dredging of Khaprabhanga Chapalir Don River in Patuakhali District for Improvement of Navigability IOSR Journal of Engineering (IOSRJEN) ISSN (e): 2250-3021, ISSN (p): 2278-8719 Vol. 04, Issue 06 (June. 2014), V3 PP 32-38 www.iosrjen.org Feasibility Study for Dredging of Khaprabhanga Chapalir Don River

More information

ISOLATION OF NON-HYDROSTATIC REGIONS WITHIN A BASIN

ISOLATION OF NON-HYDROSTATIC REGIONS WITHIN A BASIN ISOLATION OF NON-HYDROSTATIC REGIONS WITHIN A BASIN Bridget M. Wadzuk 1 (Member, ASCE) and Ben R. Hodges 2 (Member, ASCE) ABSTRACT Modeling of dynamic pressure appears necessary to achieve a more robust

More information

Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean.

Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean. Ocean Motion Met 101: Introduction to the World's Oceans Produced by The COMET Program Geography: Name Pd. Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all

More information

(Refer Slide Time: 0:36)

(Refer Slide Time: 0:36) Port and Harbour Structures. Professor R. Sundaradivelu. Department of Ocean Engineering. Indian Institute of Technology, Madras. Module-2. Lecture-8B. Wave Rose Diagram. (Refer Slide Time: 0:36) We will

More information

Pathways and Effects of Indonesian Throughflow water in the Indian Ocean using Trajectory and Tracer experiments in an OGCM

Pathways and Effects of Indonesian Throughflow water in the Indian Ocean using Trajectory and Tracer experiments in an OGCM Pathways and Effects of Indonesian Throughflow water in the Indian Ocean using Trajectory and Tracer experiments in an OGCM Vinu K V Ph.D Student Division of Ocean And Atmospheric Sciences, Hokkaido University,

More information

ENSO and monsoon induced sea level changes and their impacts along the Indian coastline

ENSO and monsoon induced sea level changes and their impacts along the Indian coastline Indian Journal of Marine Sciences Vol. 35(2), June 2006, pp. 87-92 ENSO and monsoon induced sea level changes and their impacts along the Indian coastline O.P.Singh* Monsoon Activity Centre, India Meteorological

More information

Appendix E Cat Island Borrow Area Analysis

Appendix E Cat Island Borrow Area Analysis Appendix E Cat Island Borrow Area Analysis ERDC/CHL Letter Report 1 Cat Island Borrow Area Analysis Multiple borrow area configurations were considered for Cat Island restoration. Borrow area CI1 is located

More information

FIELD MEASUREMENTS OF SURFACE SUSPENDED SEDIMENT CONCENTRATION IN THE YANGTZE ESTUARY, CHINA

FIELD MEASUREMENTS OF SURFACE SUSPENDED SEDIMENT CONCENTRATION IN THE YANGTZE ESTUARY, CHINA International Conference on Estuaries and Coasts November 9-11, 2003, Hangzhou, China FIELD MEASUREMENTS OF SURFACE SUSPENDED SEDIMENT CONCENTRATION IN THE YANGTZE ESTUARY, CHINA Qing HE, Zhiying YU, Yuanye

More information

Tidal regime along Vietnam coast under impacts of sea level rise

Tidal regime along Vietnam coast under impacts of sea level rise VNU Journal of Science, Earth Sciences 28 (2012) 133-139 Tidal regime along Vietnam coast under impacts of sea level rise Tran Thuc, Duong Hong Son* Vietnam Institute of Meteorology, Hydrology and Environment

More information

APPLICATION OF SOUND PROPAGATION (IN THE PERSIAN GULF AND OMAN SEA)

APPLICATION OF SOUND PROPAGATION (IN THE PERSIAN GULF AND OMAN SEA) APPLICATION OF SOUND PROPAGATION (IN THE PERSIAN GULF AND OMAN SEA) Seyed Majid Mosaddad Department of Physics, Shoushtar Branch, Islamic Azad University, Shoushtar, Iran Email: mosaddad5@gmail.com Abstract

More information

Name Class Date. Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.

Name Class Date. Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used. Assessment Chapter Test B The Movement of Ocean Water USING KEY TERMS Use the terms from the following list to complete the sentences below. Each term may be used only once. Some terms may not be used.

More information

CHAPTER 8 ASSESSMENT OF COASTAL VULNERABILITY INDEX

CHAPTER 8 ASSESSMENT OF COASTAL VULNERABILITY INDEX 124 CHAPTER 8 ASSESSMENT OF COASTAL VULNERABILITY INDEX 8.1 INTRODUCTION In order to assess the vulnerability of the shoreline considered under this study against the changing environmental conditions,

More information

DUXBURY WAVE MODELING STUDY

DUXBURY WAVE MODELING STUDY DUXBURY WAVE MODELING STUDY 2008 Status Report Duncan M. FitzGerald Peter S. Rosen Boston University Northeaster University Boston, MA 02215 Boston, MA 02115 Submitted to: DUXBURY BEACH RESERVATION November

More information

Crashing waves are a sight to watch. M. J. VARKEY sheds light on how these waves are formed

Crashing waves are a sight to watch. M. J. VARKEY sheds light on how these waves are formed BIMAN BASU Crashing waves are a sight to watch. M. J. VARKEY sheds light on how these waves are formed SCIENCE REPORTER [9] MAY 1996 OU are on a seashore on a windless day. Watch the sea for some time

More information

DELHI PUBLIC SCHOOL TAPI

DELHI PUBLIC SCHOOL TAPI DELHI PUBLIC SCHOOL TAPI CLASS VII Learning Partnership 5 (KEY) Water : LESSON 5: Water (KEY) Writing Task: W.B (pp-136) 1. What are the 3 main process involved in the water cycle. Evaporation, Condensation,

More information

MESSOLOGI LAGOON AREA (GREECE)

MESSOLOGI LAGOON AREA (GREECE) MESSOLOGI LAGOON AREA (GREECE) 20 Contact: Kyriakos SPYROPOULOS TRITON Consulting Engineers 90 Pratinou Str. 11634 Athens (GREECE) Tel: +32 10 729 57 61 Fax: +32 10 724 33 58 e-mail: kspyropoulos@tritonsa.gr

More information

Oceans Humans both depend on it and threaten it with their activities

Oceans Humans both depend on it and threaten it with their activities Oceans Humans both depend on it and threaten it with their activities Oceans Water covers nearly ¾ of the Earth s surface More than 50% of the world s population lives within an hour of the coast Oceans

More information

TERMINALE DI RICEZIONE E RIGASSIFICAZIONE GAS NATURALE LIQUEFATTO (GNL) TARANTO STUDIO DI IMPATTO AMBIENTALE (SIA) ALLEGATO 15.2

TERMINALE DI RICEZIONE E RIGASSIFICAZIONE GAS NATURALE LIQUEFATTO (GNL) TARANTO STUDIO DI IMPATTO AMBIENTALE (SIA) ALLEGATO 15.2 TERMIALE DI RICEZIOE E RIGASSIFICAZIOE GAS ATURALE LIQUEFATTO (GL) TARATO STUDIO DI IMPATTO AMBIETALE (SIA) ALLEGATO 15.2 documento Foglio Rev: documento Cliente.: 03255-E&E-R-0-001 1 di 1 0 1 ALLEGATO

More information

DEVELOPMENT OF NATIONAL ABILITY TO RESPOND TO SPILLAGES OF OIL AND OTHER HARMFUL SUBSTANCES

DEVELOPMENT OF NATIONAL ABILITY TO RESPOND TO SPILLAGES OF OIL AND OTHER HARMFUL SUBSTANCES HELCOM RECOMMENDATION 31/1 (supersedes HELCOM Recommendations 1/7, 4/3 and 11/13) Adopted 4 March 2010 having regard to Article 20, Paragraph 1 b) of the Helsinki Convention DEVELOPMENT OF NATIONAL ABILITY

More information

Section Decanting Response Tool

Section Decanting Response Tool Section 9411 Decanting Response Tool T able of Contents Section Page 9411 Decanting Response Tool... 9411-1 9411.1 Introduction... 9411-1 9411.2 Decanting Policy... 9411-1 9411.2.1 Criteria... 9411-1 9411.2.2

More information

SEA SURFACE TEMPERATURE RETRIEVAL USING TRMM MICROWAVE IMAGER SATELLITE DATA IN THE SOUTH CHINA SEA

SEA SURFACE TEMPERATURE RETRIEVAL USING TRMM MICROWAVE IMAGER SATELLITE DATA IN THE SOUTH CHINA SEA SEA SURFACE TEMPERATURE RETRIEVAL USING TRMM MICROWAVE IMAGER SATELLITE DATA IN THE SOUTH CHINA SEA Mohd Ibrahim Seeni Mohd and Mohd Nadzri Md. Reba Faculty of Geoinformation Science and Engineering Universiti

More information

6.28 PREDICTION OF FOG EPISODES AT THE AIRPORT OF MADRID- BARAJAS USING DIFFERENT MODELING APPROACHES

6.28 PREDICTION OF FOG EPISODES AT THE AIRPORT OF MADRID- BARAJAS USING DIFFERENT MODELING APPROACHES 6.28 PREDICTION OF FOG EPISODES AT THE AIRPORT OF MADRID- BARAJAS USING DIFFERENT MODELING APPROACHES Cecilia Soriano 1, Darío Cano 2, Enric Terradellas 3 and Bill Physick 4 1 Universitat Politècnica de

More information

DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT

DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT 10 th Wind Energy Conference DEWEK 2010 DIRECTION DEPENDENCY OF OFFSHORE TURBULENCE INTENSITY IN THE GERMAN BIGHT Annette Westerhellweg, Beatriz Canadillas, Thomas Neumann DEWI GmbH, Wilhelmshaven, Germany,

More information

Artificial headlands for coastal restoration

Artificial headlands for coastal restoration Artificial headlands for coastal restoration J. S. Mani Professor, Department of Ocean Engineering, Indian Institute of Technology Madras, Chennai 636, India Abstract Construction of a satellite harbour

More information

COASTAL EROSION: INVESTIGATIONS IN THE SOUTHWEST COAST OF SRI LANKA

COASTAL EROSION: INVESTIGATIONS IN THE SOUTHWEST COAST OF SRI LANKA COASTAL EROSION: INVESTIGATIONS IN THE SOUTHWEST COAST OF SRI LANKA Wijayawardane I.S.K. 1, Ansaf K.M.M. 2, Ratnasooriya A.H.R. 3, Samarawickrama S.P. 4 1,2 Postgraduate Student, Department of Civil Engineering,

More information

Section Decanting Response Tool

Section Decanting Response Tool Section 9411 Decanting Response Tool T able of Contents Section Page 9411 Decanting Response Tool... 9411-1 9411.1 Introduction... 9411-1 9411.2 Decanting Policy... 9411-1 9411.2.1 Criteria... 9411-1 9411.2.2

More information

Effect of sea surface temperature on monsoon rainfall in a coastal region of India

Effect of sea surface temperature on monsoon rainfall in a coastal region of India Loughborough University Institutional Repository Effect of sea surface temperature on monsoon rainfall in a coastal region of India This item was submitted to Loughborough University's Institutional Repository

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 8 March 2010

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 8 March 2010 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 8 March 2010 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

3 The monsoon currents in an OGCM

3 The monsoon currents in an OGCM 3 The monsoon currents in an OGCM The observations show that both Ekman drift and geostrophy contribute to the surface circulation in the north Indian Ocean. The former decays rapidly with depth, but the

More information

SEASONAL SEA LEVEL VARIABILITY AND ANOMALIES IN THE SINGAPORE STRAIT

SEASONAL SEA LEVEL VARIABILITY AND ANOMALIES IN THE SINGAPORE STRAIT Proceedings of International Conference in Ocean Engineering, ICOE Proceedings 2009 of ICOE 2009 Seasonal IIT sea Madras, level Chennai, variability India. and anomalies in the Singapore Strait 1-5 Feb.

More information

Technical Brief - Wave Uprush Analysis Island Harbour Club, Gananoque, Ontario

Technical Brief - Wave Uprush Analysis Island Harbour Club, Gananoque, Ontario Technical Brief - Wave Uprush Analysis RIGGS ENGINEERING LTD. 1240 Commissioners Road West Suite 205 London, Ontario N6K 1C7 October 31, 2014 Table of Contents Section Page Table of Contents... i List

More information

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture!

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture! Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction Previous Lecture! Global Winds General Circulation of winds at the surface and aloft Polar Jet Stream Subtropical Jet Stream Monsoons 1 2 Radiation

More information

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are.

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. 1. A cool breeze is blowing toward the land from the ocean on a warm, cloudless summer day. This condition is

More information

Systematic Validation of Conductivity and Temperature from Ocean moored buoy data in the northern Indian Ocean with in situ ship based measurements

Systematic Validation of Conductivity and Temperature from Ocean moored buoy data in the northern Indian Ocean with in situ ship based measurements Indian Journal of Geo-Marine Sciences Vol. 45(2), February 2016, pp. 224-229 Systematic Validation of Conductivity and Temperature from Ocean moored buoy data in the northern Indian Ocean with in situ

More information

Synthesis of marine debris modeling and observations: recent progress in understanding and applications

Synthesis of marine debris modeling and observations: recent progress in understanding and applications 2016 New Year Symposium on Marine Litter Ministry of the Environment, Government of Japan, Tokyo University of Marine Science and Technology, January 23-24, 2016 Synthesis of marine debris modeling and

More information

Taranaki Tsunami Inundation Analysis. Prepared for Taranaki Civil Defence Emergency Management Group. Final Version

Taranaki Tsunami Inundation Analysis. Prepared for Taranaki Civil Defence Emergency Management Group. Final Version Taranaki Tsunami Inundation Analysis Prepared for Taranaki Civil Defence Emergency Management Group Final Version June 2012 AM 12/07 HBRC Plan Number 4362 Asset Management Group Technical Report Prepared

More information

Understanding of Meteorology. for. Handling LNG at Ports

Understanding of Meteorology. for. Handling LNG at Ports Understanding of Meteorology for Handling LNG at Ports All environmental forces on the berth and the berthed ship are considered. When evaluating environmental forces, first estimates are obtained for

More information

APPENDIX H PLUME MODELS

APPENDIX H PLUME MODELS APPENDIX H PLUME MODELS APPENDIX H PLUME MODELS Prior to the initiation of recovery activities, the National Oceanic and Atmospheric Administration ran a series of oil plume trajectory analyses (2001a)

More information

The events associated with the Great Tsunami of 26 December 2004 Sea Level Variation and Impact on Coastal Region of India

The events associated with the Great Tsunami of 26 December 2004 Sea Level Variation and Impact on Coastal Region of India The events associated with the Great Tsunami of 26 December 2004 Sea Level Variation and Impact on Coastal Region of India Satish R. Shetye National Institute of Oceanography, Goa Tsunamis are shallow-water

More information

Applications of Collected Data from Argos Drifter, NOAA Satellite Tracked Buoy in the East Sea

Applications of Collected Data from Argos Drifter, NOAA Satellite Tracked Buoy in the East Sea Applications of Collected Data from Argos Drifter, NOAA Satellite Tracked Buoy in the East Sea Young-Sang Suh (yssuh@nfrdi.re.kr) Ocean Research Team, National Fisheries Research and Development Institute,

More information

Development of an Oil Delivery System to Create Neutrally Buoyant Oil Plumes

Development of an Oil Delivery System to Create Neutrally Buoyant Oil Plumes 2014 Conference and Exhibition Development of an Oil Delivery System to Create Neutrally Buoyant Oil Plumes Bill Schmidt, Program Manager Dave DeVitis, Test Director MAR Incorporated Acknowledgements U.S.

More information

INCLINOMETER DEVICE FOR SHIP STABILITY EVALUATION

INCLINOMETER DEVICE FOR SHIP STABILITY EVALUATION Proceedings of COBEM 2009 Copyright 2009 by ABCM 20th International Congress of Mechanical Engineering November 15-20, 2009, Gramado, RS, Brazil INCLINOMETER DEVICE FOR SHIP STABILITY EVALUATION Helena

More information

SURFACE CURRENTS AND TIDES

SURFACE CURRENTS AND TIDES NAME SURFACE CURRENTS AND TIDES I. Origin of surface currents Surface currents arise due to the interaction of the prevailing wis a the ocean surface. Hence the surface wi pattern (Figure 1) plays a key

More information

INUNDATION, RUN-UP HEIGHTS, CROSS-SECTION PROFILES AND LITTORAL ENVIRONMENT ALONG THE TAMIL NADU COAST AFTER 26 TH DECEMBER 2004 TSUNAMI

INUNDATION, RUN-UP HEIGHTS, CROSS-SECTION PROFILES AND LITTORAL ENVIRONMENT ALONG THE TAMIL NADU COAST AFTER 26 TH DECEMBER 2004 TSUNAMI INUNDATION, RUN-UP HEIGHTS, CROSS-SECTION PROFILES AND LITTORAL ENVIRONMENT ALONG THE TAMIL NADU COAST AFTER 26 TH DECEMBER 2004 TSUNAMI D. ILANGOVAN, S. JAYAKUMAR, R. GOWTHAMAN, G. TIRODKAR, P. GANESHAN,

More information

LONG- TERM CHANGE IN PRE- MONSOON THERMAL INDEX OVER CENTRAL INDIAN REGION AND SOUTH WEST MONSOON VARIABILITY

LONG- TERM CHANGE IN PRE- MONSOON THERMAL INDEX OVER CENTRAL INDIAN REGION AND SOUTH WEST MONSOON VARIABILITY LONG- TERM CHANGE IN PRE- MONSOON THERMAL INDEX OVER CENTRAL INDIAN REGION AND SOUTH WEST MONSOON VARIABILITY *S.S. Dugam Indian Institute of Tropical Meteorology, Pune-411008 *Author for Correspondence

More information

Current mooring observations in the area of the South Kuril Islands

Current mooring observations in the area of the South Kuril Islands Current mooring observations in the area of the South Kuril Islands Georgy Shevchenko, Gennady Kantakov 2* and Valery Chastikov 2 Institute of Marine Geology and Geophysics FEB RAS, Yuzhno-Sakhalinsk,

More information

Geostrophic and Tidal Currents in the South China Sea, Area III: West Philippines

Geostrophic and Tidal Currents in the South China Sea, Area III: West Philippines Southeast Asian Fisheries Development Center Geostrophic and Tidal Currents in the South China Sea, Area III: West Philippines Anond Snidvongs Department od Marine Science, Chulalongkorn University, Bangkok

More information

General Oceanography Geology 105 Expedition #19 The Ocean and Climate

General Oceanography Geology 105 Expedition #19 The Ocean and Climate General Oceanography Geology 105 Expedition #19 The Ocean and Climate Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank answers

More information

Chapter 10 Lecture Outline. The Restless Oceans

Chapter 10 Lecture Outline. The Restless Oceans Chapter 10 Lecture Outline The Restless Oceans Focus Question 10.1 How does the Coriolis effect influence ocean currents? The Ocean s Surface Circulation Ocean currents Masses of water that flow from one

More information

Upstream environment for SBI - Modeled and observed biophysical conditions in the northern Bering Sea

Upstream environment for SBI - Modeled and observed biophysical conditions in the northern Bering Sea Upstream environment for SBI - Modeled and observed biophysical conditions in the northern Bering Sea Jaclyn Clement 1, Wieslaw Maslowski 1, Lee Cooper 2, Jacqueline Grebmeier 2, Waldemar Walczowski 3,

More information

Tides. Tides: longest waves. or seas. or ripples

Tides. Tides: longest waves. or seas. or ripples Tides or ripples or seas Tides: longest waves Tides Definition: The rise and fall of sea level due to the gravitational forces of the Moon and Sun and the rotation of the Earth. Why tides are important?

More information

Wave Transformation along Southwest coast of India using MIKE 21

Wave Transformation along Southwest coast of India using MIKE 21 23 Wave Transformation along Southwest coast of India using MIKE 21 Parvathy K.G. 1, Deepthi I. Gopinath 2, Noujas V. 3 and K. V. Thomas 3 1 National Institute of Technology Karnataka, Surathkal, 575025,

More information

Lecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 15 Earth Science, 12e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 15 Earth Science, 12e Tarbuck/Lutgens 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information