Contamination of Bourgas Port Waters with Oil
|
|
- Jerome Webb
- 6 years ago
- Views:
Transcription
1 Contamination of Bourgas Port Waters with Oil Vasko Galabov (1), Anna Kortcheva (1,2), Georgi Kortchev (1,3) and Jordan Marinski (1,4) (1) National Institute of Meteorology and Hydrology, Bulgarian Academy of Sciences, 1784 Sofia, Bulgaria Tel: Vasko.Galabov@meteo.bg (2) Tel: Anna.Kortcheva@ meteo.bg (3) Tel: Georgi.Kortchev@ meteo.bg (4) Tel: marinski@bas.bg Abstract Accurate prediction of the behavior of oil pollution is crucial for successful decision making and planning of operations to combat pollution of the coastal zone to protect the environment. In addition, the oil spills in the Bourgas Bay of West Black Sea may cause extra contamination of port waters in different terminals of Port of Bourgas with oil and liquid dangerous products which is extremely undesirable from the environmental point of view. The present study aims to assess the impact of the risk of oil spills in the auquatory of Bourgas Port and to determine potentially dangerous areas of contamination in the inner basins of the port and the conditions for their occurrence. The numerical model MOTHY, developed by Météo-France, have been used to predict the drift of pollutants on the sea surface. Numerical simulations are carried out in the Bourgas bay and harbor waters for potential and real oil spill accidents. The range of hypothetical scenarios includes various winds and current conditions. The simulation results indicate the places with a high risk of oil pollution in the port of Bourgas. The proposed methodology utilized in this study is applicable to risk assessments for other ports and coastal areas potentially affected by floating pollutants.
2 Introduction Port of Bourgas is located in the Bourgas Bay that is the widest bay in the western part of the Black Sea. Set deep into the mainland, the bay includes the westernmost point (27º26 54 ) of the Black Sea. The Bourgas Bay is 41 km at its widest part and 25 m at its deepest, reaching 31 km at its greatest innermost extent, and 750 km 2 area, approximately. The Port Bourgas is the biggest port in Bulgaria and it is a key-point of Trans border Corridor 8, ensures direct access to the Black Sea of Southern Italian ports. For this reason the Port of Bourgas is chosen as a pilot site in two South East European projects ECOPORT 8 and TEN ECOPORT ( and the present study is a part of them. According to BG Ministry of transport, Bourgas port,is divided the following terminals: East, Bulk cargoes, Bulk terminal 2A, West, Oil terminal Rossenetz and passenger terminals in Nesebar and Sozopol (Fig. 1). Port activities /in public and private terminals and ports/ interact with activities of adjacent industrial zones around Bourgas Bay and current environment conditions of Bourgas Port are very complicated. The crude oil and oil products terminal Rossenetz has been built about 3 miles southeast of the existing East and West Terminals and its activities are supposed to be one of the main sources for contamination of port waters (internal basins 1, 2, 3 and 4) with oil and oil products. Fig. 1: Location of Bourgas Port terminals
3 It is supposed that the oil spills in the Bourgas Bay may cause extra contamination of port waters in different terminals of the Bourgas port with oil and liquid dangerous products, which is extremely undesirable from an environmental point of view and with respect to the forthcoming certification of the Bourgas port. A powerful tool for determining any potentially dangerous areas of contamination in the inner basins of the port and its terminals is to use the numerical modeling and simulation of the behavior of oil spills in coastal waters. Oil spills in the Bay of Bourgas can be caused by the tankers that deliver the product to the oil terminal Rossenetz of the Bourgas Port supplying LUKOIL refinery with crude oil. To minimize the damage resulting from oil spill accidents, it is necessary to respond quickly with an appropriate strategy. Accurately forecasting the behavior of the spilled oil is crucial for a successful recovery operation and protection of the marine resources. It is also important to simulate the most probable scenarios (i.e. locations on the tanker routes and different weather conditions and circulation within the bay) in order to have a better preparedness and to choose the right positions of the monitoring facilities. Therefore, the numerical modeling and simulation of the spilled oil at sea plays an important role in the oil spill response and contingency decision-making. The study of the effects of the potential oil pollution for the port of Bourgas terminals includes determination of the potentially affected areas of the port waters. Model description Lagrangian trajectory modeling: floating pollutants spread model The oil drift forecast is carried out by means of a numerical model, named MOTHY, describing the ocean dynamics and the physicochemical behavior of the pollutant. The numerical model MOTHY has been developed by the Marine Forecast Division of Meteo-France and implemented for the Black Sea. (Daniel, et al, 1999, 2005, Kortchev et al, 1999). The model MOTHY uses the Langragian approach, trajectories based on the assumption that the oil can be idealized by a large number of particles that move by advection, turbulent dispersion and oil spreading dynamics. Barotropic model MOTHY model system consists of a model for the wind currents and a model for the oil spill drift prediction. The wind currents are computed by a barotropic model coupled with a turbulent model and driven by the wind and mean sea level pressure output from an atmospheric model (global scale or high resolution regional scale). The barotropic model is two-dimensional, coupled with a one-dimensional for the vertical structure of the currents, therefore the wind currents model is 2.5 dimensional depth-integrated and solves the shallow water equations on a regular grid: q 1 q. q f. kq g. Pa ( s b) A. t. H 2 q (1)
4 ( H. q) 0 t (2) where t is the time, q- depth integrated current, η is the sea surface elevation, H- the total depth, f- the Coriolis parameter, k- the unit vector in the vertical, P a is the mean sea level pressure, s is the surface wind stress, b is the bottom friction stress, is the water density, g the gravitational acceleration and A the horizontal diffusion coefficient. These equations are solved by a forward in time integration in Arakawa C-grid, using a finite split-explicit difference scheme. The surface wind stress is calculated by using a quadratic relation (3):. C. W. W sx a d 10 10x. C. W. W sy a d y (3) where W, W are the horizontal components of wind at 10 m above the sea surface, a 10x 10y is the air density and C d is the drag coefficient, calculated by using the relation (4): (4) The bottom stress is calculated as: ( U V ) 1/ U (5) bx C b... V (6) by 2 2 1/ 2 C b.( U ) Here C b is the bottom friction coefficient (the value is in our case). The boundary conditions are: at the bottom the normal component of the current is 0 and at the surface condition for the gravitational waves. Oil spill drift model The second component of the system is the oil spill drift model. The oil spill is modeled as an ensemble of independent droplets, moving in response to shear current, turbulence and buoyancy. The shear current is calculated for each droplet by a bilinear eddy viscosity model. The vertical eddy viscosity in the model increases linearly with the distance from the sea surface and the bottom (Poon and Madsen, 1991). The governing equation is: w 1 P i f w t t n z w z (7)
5 where w=u+i.v is the horizontal current velocity, t is the eddy viscosity. The turbulent diffusion is represented by three-dimensional random walk technique. For one time step t, the motion is: D R 2 K t h h in direction: 2 R (8) where K h is the horizontal diffusion coefficient and R- random number between 0 and 1 In the vertical, the motion is: D R v Kv t (9) where K v is the vertical diffusion coefficient. The buoyancy depends on the density and size of the droplet, so the larger ones are more buoyant and tend to remain on the surface, while the smaller are mixed downward. U f The vertical speed U f is determined by (10) and (11) (Elliot et al, 1986): 2 0 g d ( 1 ) For small droplets d d c (10) Uf gd ( 1 ) 3 For large droplets d d c (11) where the critical diameter d c is: d c 3 9, g( 1 ) is the sea water density and viscosity. If a droplet is moved on the land, then it is considered beached and takes no further part of the simulation. (12) Water circulation in the Bourgas Bay geophysical hydrodynamic model The water circulation in the Bourgas Bay and character of sea currents is determined by geophysical hydrodynamic non-stationary 3D numerical model created in the Institute of Numerical Mathematics (Sarkisyan A., 1977) and developed in the Institute of Oceanology, Varna (Trukhchev et al., 1995, 2004 ). The initial system includes equations and boundary conditions, which are traditional for a model of ocean hydrothermodynamics; their finite-difference approximation is based on the balance of properties within the "boxes" on Arakawa B-grid. The modeling computations of Bourgas
6 Bay currents represent the character of circulation in the bay. The results show the presence of a developed eddy structure of the currents and the existence of rapid adjustment (of several hours) of the movements to the changes in the field of wind. As a rule, in the Small Bourgas bay there forms one main vortex: during north, northeast and east winds the system of currents is cyclonal, and during west, southwest and south winds anticyclonal, Fig 2. Fig.2: Cyclonal (a) and anti-cyclonal (b) type of circulation [cm/s] in Bourgas Bay The cyclonal type of movements is usually dominating. In the water areas immediately close to the coast, coastal jets and small scale eddies are formed. In our study the monthly mean climatic fields of the sea current in the Bourgas Bay are calculated because the anti-cyclonical appears mainly when the wind is from the southwestern quadrant and it such situation the winds and currents are typically much weaker, therefore this case is not of much significance for our study goals. Two-dimensional simulation of oil spills and localization of oil pollution in port This study summarizes the results of the hypothetical oil spill simulations in the Bourgas Bay, the objective of which is to localize oil pollution in internal port water basins 1,2,3 and 4 and to estimate the risk of oil-spill contact to the shoreline in the port terminals and harbor structures, (breakwaters and ship berth quay walls). Forecasts strongly depend on the initial conditions, and therefore on the position of the slicks. Based on the identified spill scenarios and type of oil, oil drift modeling can be done using any combination of release rates and durations. In order to capture the wind and ocean current variations, typically simulations are performed using historical wind conditions and monthly averaged permanent currents direction and speed. The study of trajectories (oil drift) consisted of simulations of a large number of scenarios of combination of incident type, current field and local winds in the Bourgas bay. The oil spill
7 model MOTHY calculates the spreading and diffusion and slick drift of an oil particle at the water surface due to the winds, waves and currents. Scenarios covered spills of the oil type Bunker fuel (Fuel oil No. 6); the oil density was chosen to be 930 kg/m3; the duration of the release 4 hours, the durations of the spill simulations up to 168 hours (7 days). Numerical simulations are carried out in Bourgas Bay for potential and real oil accidents. The range of hypothetical scenarios includes various wind and current conditions. The points of release for the simulations are chosen along the main tanker routes (fairway) to the terminals of Port Bourgas. Also taken into account is the possibility of pollution due to a release of fuel from other type of ship. The numerical simulations were carried out for the area of the Bourgas bay and port waters for 20 locations imitating potential and real oil accidents along the main (existing) traffic route (corridor) to the port of Bourgas (terminal East, terminal 2A, terminal West ) and near to the Oil terminal Rosenetz. The range of the hypothetical scenarios includes various wind and current conditions. The starting points for the simulations are chosen along the main transport route (fairway) to the terminals of the port of Bourgas. Input data for MOTHY model are bathymetry, monthly mean climatic fields of the sea currents in the Bourgas bay calculated by the hydrodynamic non-stationary 3D numerical model, wind and mean sea level pressure fields. The simulations yielded the following area oiling results: In case of an accident in the area of roadsteads or in the area of the approach channel (external port waters) the simulations show that there is a risk for oil pollution mainly for the internal basin 2, fig 3. In case of oil pollution simulation with sources in small Bourgas bay the simulation output shows that the internal basins 2, 3 and 4 are affected by significant oil pollution in various meteorological conditions. The basin 1 of the terminal East (the old harbor of Bourgas) is not affected by oil pollution. A pollution of this terminal occurs only in a case of accidents inside the harbor. In case of an accident east of the roadsteads (east of the oil terminal Rosenetz) the probability for pollution of the terminals in the Bourgas port is much lower and is negligible. Because the main route of the tanker ships is east of Rosenetz (where there is some chance of a big oil accident) the terminals and port waters in basins 1,2,3 and 4 are well protected against such accidents. Taking into account analyses of all results, obtained by processing a large number of simulations we can summarize the results and state locations and areas with different level of oil risk pollution in port waters, Fig. 4.
8 Fig.3: Oil pollution in port waters when oil drift source is located on access channel - locations of oil pollution Fig.4: The zones in port at risk of oil pollution: - area with significant risk will be affected in any conditions; - area with average risk depending on predominant conditions (winds and currents); - area with not negligible risk during the specific meteorological conditions;
9 Conclusions The modeling results present a range of useful information on potential oil movement and behavior in Bourgas Bay and Port of Bourgas. It should be remembered that these results are based on probabilities and that the exact areas, oiled and travel times and locations cannot be predicted with complete accuracy. Modeling can be a very useful response tool but should be used in conjunction with all other available information. Acknowledgements This research was made possible thanks to a research grant provided by South East Europe Transnational Cooperation Program within Transnational enhancement of ECOPORT 8 network - TEN ECOPORT project Code SEE/D/189/2.2/X References Daniel P. (1999). Marine pollution transport modeling. In: Proceedings of Marpolser 98, WMO/TD No960, Daniel P., Josse P.and Danadin P. (2005), Further improvement of drift forecast at sea based on operational oceanography systems. In:Coastal Engineering VII, Modelling, Measurements, Engineering and Management of Seas and Coastal Regions, Elliot A.J., Hurford N. and Penn C.J. (1986), Shear Diffusion and the Spreading of Oil Slicks Marine Pollution Bulletin, Pergamon Journals Ltd., 17, (7), Kortchev G., Mungov G., Kortcheva A.and P. Daniel (1999), Operational Forecasting of oil spill drift in the Black Sea, In: Proc. Oceanogpraphy of the Eastern Mediterranean and Black Sea, Zappeion International Conference, Atthens, Greece, 26 February, 1999, Poon Y.K. and O.S. Madsen, 1991: A two layers wind driven coastal circulation model, J. Geophys. Res., 96, (C2), Sarkisyan A. (1977), The Diagnostic Calculation of a Large Scale Oceanic Circulation. In: The Sea, Marine Modeling. New York, 6, Trukhchev D., Ivanov D., Ibrayev R., Patzireva T. and Rabie A. (2004), Hydrophysical Study of Bourgas Bay. Modelling the Synoptic Circulation Patterns. Comptes Rendus de l'academie Bulgare des Sciences, 57, (3), Keywords: marine pollution, oil spill, numerical simulations, port waters, Black Sea
PAJ Oil Spill Simulation Model for the Sea of Okhotsk
PAJ Oil Spill Simulation Model for the Sea of Okhotsk 1. Introduction Fuji Research Institute Corporation Takashi Fujii In order to assist in remedial activities in the event of a major oil spill The Petroleum
More informationPREDICTION OF OIL SPILL TRAJECTORY WITH THE MMD-JMA OIL SPILL MODEL
PREDICTION OF OIL SPILL TRAJECTORY WITH THE MMD-JMA OIL SPILL MODEL Project Background Information MUHAMMAD HELMI ABDULLAH MALAYSIAN METEOROLOGICAL DEPARTMENT(MMD) MINISTRY OF SCIENCE, TECHNOLOGY AND INNOVATION
More informationAN INTEGRATED MODELING APPROACH FOR SIMULATING OIL SPILL AT THE STRAIT OF BOHAI SEA. Jinhua Wang 1 and Jinshan Zhang 1
AN INTEGRATED MODELING APPROACH FOR SIMULATING OIL SPILL AT THE STRAIT OF BOHAI SEA Jinhua Wang 1 and Jinshan Zhang 1 A three dimensional integrated model is developed for simulating oil spills transport
More informationHORIZONTAL TURBULENT DIFFUSION AT SEA SURFACE FOR OIL TRANSPORT SIMULATION
HORIZONTAL TURBULENT DIFFUSION AT SEA SURFACE FOR OIL TRANSPORT SIMULATION Yoshitaka Matsuzaki 1, Isamu Fujita 2 In numerical simulations of oil transport at the sea surface, it is not known how to determine
More informationPETROLEUM HAZARDS MANAGEMENT BY GEOMATIC SYSTEMS
PETROLEUM HAZARDS MANAGEMENT BY GEOMATIC SYSTEMS H. ASSILZADEH Spatial Information Technology & Engineering (SITE) Research Center Faculty of Engineering, Universiti Putra Malaysia, 43400 UPM, Serdang
More informationUsing the Mercator ocean forecasting system to compute coastal maritime pollution risk indicators on the Atlantic European coasts
Environmental Problems in Coastal Regions VI 437 Using the Mercator ocean forecasting system to compute coastal maritime pollution risk indicators on the Atlantic European coasts S. Besnard 1, E. Dombrowsky
More informationOPTIMIZATION IN OIL SLICK COMBATING STATIONS ALLOCATION. APPLICATION TO THE SEA OF AZOV
Global NEST Journal, Vol 16, No 2, pp 402-410, 2014 Copyright 2014 Global NEST Printed in Greece. All rights reserved OPTIMIZATION IN OIL SLICK COMBATING STATIONS ALLOCATION. APPLICATION TO THE SEA OF
More information8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound
8.1 Attachment 1: Ambient Weather Conditions at Jervoise Bay, Cockburn Sound Cockburn Sound is 20km south of the Perth-Fremantle area and has two features that are unique along Perth s metropolitan coast
More informationADVANTAGES OF GIS-INTEGRATED MARITIME DATA IN THE BLACK SEA REGION FOR MULTIPURPOSE USE
INTERAGENCY INTERACTION IN CRISIS MANAGEMENT AND DISASTER RESPONSE 2017 ADVANTAGES OF GIS-INTEGRATED MARITIME DATA IN THE BLACK SEA REGION FOR MULTIPURPOSE USE Lyubka Pashova 1, Anna Kortcheva 2, Vasko
More informationC o a s t a l p o l l u t i o n
C o a s t a l p o l l u t i o n Copernicus for Coastal Zone Management and Marine Environment Monitoring Service Copernicus EU Copernicus EU Copernicus EU www.copernicus.eu I N T R O D U C T I O N Main
More informationStorms. 3. Storm types 4. Coastal Sectors 5. Sorm Location and Seasonality 6. Storm Severity 7. Storm Frequency and grouping 8. The design storm event
1. Introduction Storms 2. The Impact of Storms on the coast 3. Storm types 4. Coastal Sectors 5. Sorm Location and Seasonality 6. Storm Severity 7. Storm Frequency and grouping 8. The design storm event
More informationSCIENTIFIC RESEARCH AND EDUCATION IN THE AIR FORCE AFASES2017
SCIENTIFIC RESEARCH AND EDUCATION IN THE AIR FORCE AFASES2017 PROBABILITY ASSESSMENT OF POSSIBLE VOLCANIC ASH CONTAMINATION FOR THE BULGARIAN AIRSPACE BY DEVELOPING OF EVENT TREE AND RISK MATRIX FOR HYPOTHETICAL
More informationApplication and verification of ECMWF products 2013
Application and verification of EMWF products 2013 Hellenic National Meteorological Service (HNMS) Flora Gofa and Theodora Tzeferi 1. Summary of major highlights In order to determine the quality of the
More informationOperational storm surge modelling in the Western Black Sea: one way coupling with a wave model
Bulgarian Academy of Sciences Bulgarian Journal of Meteorology and Hydrology Bul. J. Meteo & Hydro 21/1-2 (2016) 10-23 National Institute of Meteorology and Hydrology Operational storm surge modelling
More informationTOSCA RESULTS OVERVIEW
TOSCA RESULTS OVERVIEW Almost 3 years after the project started, TOSCA has proved capable of improving oil spill tracking systems. TOSCA has brought updated knowledge on surface currents and noticeable
More informationOCEAN HYDRODYNAMIC MODEL
Jurnal Teknologi Pengelolaan Limbah (Journal of Waste Management Technology), ISSN 1410-9565 Volume 10 Nomor 1 Juli 2007 (Volume 10, Number 1, July, 2007) Pusat Teknologi Limbah Radioaktif (Radioactive
More informationAPPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1
APPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1 1 By David B. Fissel, Mar Martínez de Saavedra Álvarez, and Randy C. Kerr, ASL Environmental Sciences Inc. (Feb. 2012) West Greenland Seismic
More informationMARINE BOUNDARY-LAYER HEIGHT ESTIMATED FROM NWP MODEL OUTPUT BULGARIA
MARINE BOUNDARY-LAYER HEIGHT ESTIMATED FROM NWP MODEL OUTPUT Sven-Erik Gryning 1 and Ekaterina Batchvarova 1, 1 Wind Energy Department, Risø National Laboratory, DK-4 Roskilde, DENMARK National Institute
More informationMersea Oil Spill Drift Forecast Demonstrations in TOP2
Mersea Oil Spill Drift Forecast Demonstrations in TOP2 Bruce Hackett (met.no), George Zodiatis (UCY), Pierre Daniel (MeteoFrance), Francois Parthiot (Cedre) Presented at 3rd Mersea Plenary Meeting, CNR,
More informationATMOSPHERIC CIRCULATION AND WIND
ATMOSPHERIC CIRCULATION AND WIND The source of water for precipitation is the moisture laden air masses that circulate through the atmosphere. Atmospheric circulation is affected by the location on the
More informationYour web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore
Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore ISTHMU S tombolo For the complete encyclopedic entry with media resources,
More informationInternational Conference Analysis and Management of Changing Risks for Natural Hazards November 2014 l Padua, Italy
Abstract code: AO6 Hindcast of extreme hydro-meteorological events along the Bulgarian Black Sea coast Anna Kortcheva, Vasko Galabov, Marieta Dimitrova, Andrey Bogatchev National Institute of Meteorology
More informationGNOME Oil Spill Modeling Lab
GNOME Oil Spill Modeling Lab Name: Goal: After simulating an actual oil spill event, you will understand how oceanographers help to protect marine resources from pollution such as oil spills. You will
More informationModelling the Channel and the Bay of Biscay using the MARS model. Contributions: Dyneco Physed / Pelagos / Benthos EMH
Modelling the Channel and the Bay of Biscay using the MARS model Contributions: Dyneco Physed / Pelagos / Benthos EMH Overview 1. The MANGA Configuration 2. Model validation: Sea Surface Temperature 3.
More informationWater Stratification under Wave Influence in the Gulf of Thailand
Water Stratification under Wave Influence in the Gulf of Thailand Pongdanai Pithayamaythakul and Pramot Sojisuporn Department of Marine Science, Faculty of Science, Chulalongkorn University, Bangkok, Thailand
More informationApplication and verification of ECMWF products: 2010
Application and verification of ECMWF products: 2010 Hellenic National Meteorological Service (HNMS) F. Gofa, D. Tzeferi and T. Charantonis 1. Summary of major highlights In order to determine the quality
More informationAir Pollution Meteorology
Air Pollution Meteorology Government Pilots Utilities Public Farmers Severe Weather Storm / Hurricane Frost / Freeze Significant Weather Fog / Haze / Cloud Precipitation High Resolution Weather & Dispersion
More informationEnvironmental Risk from Ship traffic along the Norwegian Coast Odd Willy Brude, Det Norske Veritas, Veritasveien 1, 1322 Høvik, Norway
Environmental Risk from Ship traffic along the Norwegian Coast 15.02.2012 Odd Willy Brude, Det Norske Veritas, Veritasveien 1, 1322 Høvik, Norway Marte Braathen, Det Norske Veritas, Veritasveien 1, 1322
More informationDeveloping integrated remote sensing and GIS procedures for oil spill monitoring on the Libyan coast
Coastal Processes III 125 Developing integrated remote sensing and GIS procedures for oil spill monitoring on the Libyan coast A. Eljabri & C. Gallagher Department of Civil Engineering and Built Environment,
More informationDr Marc Lucas CLS Toulouse, France.
Dr Marc Lucas CLS Toulouse, France. Oceanology International 15th March 2012 Slide 1 Ocean depiction In the past: Information mainly comes from in situ measurements (ADCP) Now: The role of satellite data
More information1. Oceans. Example 2. oxygen.
1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital
More informationNerushev A.F., Barkhatov A.E. Research and Production Association "Typhoon" 4 Pobedy Street, , Obninsk, Kaluga Region, Russia.
DETERMINATION OF ATMOSPHERIC CHARACTERISTICS IN THE ZONE OF ACTION OF EXTRA-TROPICAL CYCLONE XYNTHIA (FEBRUARY 2010) INFERRED FROM SATELLITE MEASUREMENT DATA Nerushev A.F., Barkhatov A.E. Research and
More informationGlobal Wind Patterns
Name: Earth Science: Date: Period: Global Wind Patterns 1. Which factor causes global wind patterns? a. changes in the distance between Earth and the Moon b. unequal heating of Earth s surface by the Sun
More informationExploitation of Ocean Predictions by the Oil and Gas Industry. GODAE OceanView Symposium 2013
Exploitation of Ocean Predictions by the Oil and Gas Industry GODAE OceanView Symposium 2013 Introduction Information needs Challenges Acknowledgements IMarEST/SUT Metocean Awareness Course Colleagues
More informationOcean Mixing and Climate Change
Ocean Mixing and Climate Change Factors inducing seawater mixing Different densities Wind stirring Internal waves breaking Tidal Bottom topography Biogenic Mixing (??) In general, any motion favoring turbulent
More informationNAM-WRF Verification of Subtropical Jet and Turbulence
National Weather Association, Electronic Journal of Operational Meteorology, 2008-EJ3 NAM-WRF Verification of Subtropical Jet and Turbulence DOUGLAS N. BEHNE National Weather Service, Aviation Weather
More informationImpact of Typhoons on the Western Pacific Ocean (ITOP) DRI: Numerical Modeling of Ocean Mixed Layer Turbulence and Entrainment at High Winds
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Impact of Typhoons on the Western Pacific Ocean (ITOP) DRI: Numerical Modeling of Ocean Mixed Layer Turbulence and Entrainment
More informationSea Ice Characteristics and Operational Conditions for Ships Working in the Eastern Zone of the NSR
The Arctic 2030 Project: Feasibility and Reliability of Shipping on the Northern Sea Route and Modeling of an Arctic Marine Transportation & Logistics System 3-rd. Industry Seminar: Sea-Ice & Operational
More informationA Study on Residual Flow in the Gulf of Tongking
Journal of Oceanography, Vol. 56, pp. 59 to 68. 2000 A Study on Residual Flow in the Gulf of Tongking DINH-VAN MANH 1 and TETSUO YANAGI 2 1 Department of Civil and Environmental Engineering, Ehime University,
More informationAnnual transport rates at two locations on the fore-slope.
Sediment Transport by Currents Fore-slope Sediment transport rates and sediment concentrations were computed from the hydrodynamic model runs as well as from direct measurements of current velocities at
More informationRecap: Static Fluids
Recap: Static Fluids Archimedes principal states that the buoyant force acting on an object is equal to the weight of fluid displaced. If the average density of object is greater than density of fluid
More informationMarine Current Potential Energy for Environmental Friendly Electricity Generation in Bali, Lombok and Makassar Straits
Environmental Technology and Management Conference 2006 September 7-8, 2006 Bandung, West Java, Indonesia Marine Current Potential Energy for Environmental Friendly Electricity Generation in Bali, Lombok
More informationThe Planetary Circulation System
12 The Planetary Circulation System Learning Goals After studying this chapter, students should be able to: 1. describe and account for the global patterns of pressure, wind patterns and ocean currents
More informationLecture 14. Equations of Motion Currents With Friction Sverdrup, Stommel, and Munk Solutions Remember that Ekman's solution for wind-induced transport
Lecture 14. Equations of Motion Currents With Friction Sverdrup, Stommel, and Munk Solutions Remember that Ekman's solution for wind-induced transport is which can also be written as (14.1) i.e., #Q x,y
More information1 Executive summary. 2 Principles of SAT-OCEAN service
S SCOPE OF WORK FOR ROUTING SERVICES 1 Executive summary SAT-OCEAN has developed an innovative routing service enabling for significant time and energy savings. This solution is going beyond traditional
More informationEfficacy Evaluation of Data Assimilation for Simulation Method of Spilled Oil Drifting
Proceedings of 5th PAAMES and AMEC2012 Dec. 10-12, 2012, Taiwan Paper No. SEPAS-05 Efficacy Evaluation of Data Assimilation for Simulation Method of Spilled Oil Drifting Satoaki TSUTSUKAWA, Hiroyoshi SUZUKI
More informationQueensland Storm Surge Forecasting Model Design Using Sensitivity Analysis
21st International Congress on Modelling and Simulation, Gold Coast, Australia, 29 Nov to 4 Dec 215 www.mssanz.org.au/modsim215 Queensland Storm Surge Forecasting Model Design Using Sensitivity Analysis
More informationWQMAP (Water Quality Mapping and Analysis Program) is a proprietary. modeling system developed by Applied Science Associates, Inc.
Appendix A. ASA s WQMAP WQMAP (Water Quality Mapping and Analysis Program) is a proprietary modeling system developed by Applied Science Associates, Inc. and the University of Rhode Island for water quality
More informationAssessing Storm Tide Hazard for the North-West Coast of Australia using an Integrated High-Resolution Model System
Assessing Storm Tide Hazard for the North-West Coast of Australia using an Integrated High-Resolution Model System J. Churchill, D. Taylor, J. Burston, J. Dent September 14, 2017, Presenter Jim Churchill
More informationWINTER NIGHTTIME TEMPERATURE INVERSIONS AND THEIR RELATIONSHIP WITH THE SYNOPTIC-SCALE ATMOSPHERIC CIRCULATION
Proceedings of the 14 th International Conference on Environmental Science and Technology Rhodes, Greece, 3-5 September 2015 WINTER NIGHTTIME TEMPERATURE INVERSIONS AND THEIR RELATIONSHIP WITH THE SYNOPTIC-SCALE
More informationEFFECTIVE TROPICAL CYCLONE WARNING IN BANGLADESH
Country Report of Bangladesh On EFFECTIVE TROPICAL CYCLONE WARNING IN BANGLADESH Presented At JMA/WMO WORKSHOP ON EFFECTIVE TROPICAL CYCLONE WARNING IN SOUTHEAST ASIA Tokyo, Japan,11-14 March 2014 By Sayeed
More informationStorm surge forecasting and other Met Office ocean modelling
Storm surge forecasting and other Met Office ocean modelling EMODnet stakeholder meeting Clare O Neill + many others Outline Ocean modelling at the Met Office Storm surge forecasting Current operational
More informationGeneral Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be
General Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be a bonus) is well written (take your time to edit) shows
More informationRSMC WASHINGTON USER'S INTERPRETATION GUIDELINES ATMOSPHERIC TRANSPORT MODEL OUTPUTS
RSMC WASHINGTON USER'S INTERPRETATION GUIDELINES ATMOSPHERIC TRANSPORT MODEL OUTPUTS -Version 2.0- (January 2007) 1. Introduction In the context of current agreements between the National Oceanic and Atmospheric
More informationDynamics of the Ems Estuary
Dynamics of the Ems Estuary Physics of coastal systems Jerker Menninga 0439738 Utrecht University Institute for Marine and Atmospheric research Utrecht Lecturer: Prof. dr. H.E. de Swart Abstract During
More informationChapter 27. Shelf sea modelling Test case bohai
Chapter 27 Shelf sea modelling 27.1 Test case bohai The aim of this test case is to illustrate the use of COHERENS for tidal prediction studies, to show how an harmonic analysis can be performed and how
More informationAnnex D. Discharge Modelling Report
Annex D Discharge Modelling Report FINAL REPORT 55 Village Square Drive South Kingstown, RI 02879 Phone: +1 401 789-6224 Fax: +1 401 789-1932 www.asascience.com Oil Spill, Produced Water, Drilling Mud
More informationWind-driven Western Boundary Ocean Currents in Terran and Superterran Exoplanets
Wind-driven Western Boundary Ocean Currents in Terran and Superterran Exoplanets By Edwin Alfonso-Sosa, Ph.D. Ocean Physics Education, Inc. 10-Jul-2014 Introduction Simple models of oceanic general circulation
More informationRISK ASSESSMENT OF OIL SPILL ACCIDENTS PART 2: APPLICATION TO SARONIKOS GULF AND IZMIR BAY
Proceedings of the 13 th International Conference on Environmental Science and Technology Athens, Greece, 5-7 September 2013 RISK ASSESSMENT OF OIL SPILL ACCIDENTS PART 2: APPLICATION TO SARONIKOS GULF
More information2/15/2012. Earth System Science II EES 717 Spring 2012
Earth System Science II EES 717 Spring 2012 1. The Earth Interior Mantle Convection & Plate Tectonics 2. The Atmosphere - Climate Models, Climate Change and Feedback Processes 3. The Oceans Circulation;
More informationNewsletter # 2. Pilot sites in Greece. December 2018
A HarmonizEd framework to Mitigate coastal EroSion promoting ICZM protocol implementation Newsletter # 2 December 2018 View of a beach in Ammolofi ( Paggaio Municipality ) Pilot sites in Greece 1. Name
More informationResearch of the Influential Factors on the Simulation of Storm Surge in the Bohai Sea
Send Orders for Reprints to reprints@benthamscience.net The Open Mechanical Engineering Journal, 2014, 8, 151-156 151 Open Access Research of the Influential Factors on the Simulation of Storm Surge in
More informationCLIMATE READY BOSTON. Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016
CLIMATE READY BOSTON Sasaki Steering Committee Meeting, March 28 nd, 2016 Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016 WHAT S IN STORE FOR BOSTON S CLIMATE?
More informationStorm surges in the easternmost Gulf of Finland during operation of the Flood Protection Barrier of St. Petersburg
Storm surges in the easternmost Gulf of Finland during operation of the Flood Protection Barrier of St. Petersburg V.Ryabchenko 1, P.Andreev 2, A.Averkiev 3, A.Dvornikov 1, K.Klevanny 4, V.Tsepelev 2 1
More informationCirculation in the South China Sea in summer of 1998
Circulation in the South China Sea in summer of 1998 LIU Yonggang, YUAN Yaochu, SU Jilan & JIANG Jingzhong Second Institute of Oceanography, State Oceanic Administration (SOA), Hangzhou 310012, China;
More informationCoastal Response Research Center. Nancy Kinner University of New Hampshire (UNH) Michele Jacobi NOAA ORR. September 27, 2007
Coastal Response Research Center Nancy Kinner University of New Hampshire (UNH) Michele Jacobi NOAA ORR September 27, 2007 1 Coastal Response Research Center (CRRC) CRRC is partnership between NOAA s Office
More informationClimate Change Research Centre
Lagrangian particles to study the ocean circulation All trajectories of buoys in the Global Drifter Program Erik van Sebille With input from Matthew England, Judith Helgers, Claire Paris, Bernadette Sloyan,
More informationCHAPTER 27 AN EVALUATION OF TWO WAVE FORECAST MODELS FOR THE SOUTH AFRICAN REGION. by M. Rossouw 1, D. Phelp 1
CHAPTER 27 AN EVALUATION OF TWO WAVE FORECAST MODELS FOR THE SOUTH AFRICAN REGION by M. Rossouw 1, D. Phelp 1 ABSTRACT The forecasting of wave conditions in the oceans off Southern Africa is important
More informationEvaluating Hydrodynamic Uncertainty in Oil Spill Modeling
Evaluating Hydrodynamic Uncertainty in Oil Spill Modeling GIS in Water Resources (CE 394K) Term Project Fall 2011 Written by Xianlong Hou December 1, 2011 Table of contents: Introduction Methods: Data
More informationTHC-T-2013 Conference & Exhibition
Modeling of Shutter Coastal Protection against Storm Surge for Galveston Bay C. Vipulanandan, Ph.D., P.E., Y. Jeannot Ahossin Guezo and and B. Basirat Texas Hurricane Center for Innovative Technology (THC-IT)
More informationOcean and sea ice modeling for Arctic shipping
Ocean and sea ice modeling for Arctic shipping Mads H. Ribergaard, Till A. S. Rasmussen, Kristine S. Madsen, Ida M. Ringgaard Danish Meteorological Institute Lyngbyvej 100, Copenhagen, Denmark Ocean modelling
More informationSurface Circulation. Key Ideas
Surface Circulation The westerlies and the trade winds are two of the winds that drive the ocean s surface currents. 1 Key Ideas Ocean water circulates in currents. Surface currents are caused mainly by
More informationOn the Risk Assessment of Severe Convective Storms and Some Weather Hazards over Bulgaria ( ) - Meteorological Approach
On the Risk Assessment of Severe Convective Storms and Some Weather Hazards over Bulgaria (1991 2008) - Meteorological Approach Lilia Bocheva, Petio Simeonov, Ilian Gospodinov National Institute of Meteorology
More information16th International Conference on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes 8-11 September 2014, Varna, Bulgaria
16th International Conference on Harmonisation within Atmospheric Dispersion Modelling for Regulatory Purposes 8-11 September 2014, Varna, Bulgaria INVESTIGATION OF THE DISPERSION OF AIR POLLUTANTS BY
More informationGoals of this Chapter
Waves in the Atmosphere and Oceans Restoring Force Conservation of potential temperature in the presence of positive static stability internal gravity waves Conservation of potential vorticity in the presence
More informationTropical Update. 5 AM EDT Thursday, September 7, 2017 Hurricane Irma, Hurricane Jose, and Hurricane Katia
Tropical Update 5 AM EDT Thursday, September 7, 2017 Hurricane Irma, Hurricane Jose, and Hurricane Katia This update is intended for government and emergency response officials, and is provided for informational
More informationWIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM
WIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM PETER C. CHU, PATRICE PAULY Naval Postgraduate School, Monterey, CA93943 STEVEN D. HAEGER Naval Oceanographic Office, Stennis Space Center MATHEW
More information5 Atmospheric Disturbances 7 1.Cyclones- tropical and temperate and associated weather conditions. 2.Anticyclones and associated weather conditions.
5 Atmospheric Disturbances 7 1.Cyclones- tropical and temperate and associated weather conditions. 2.Anticyclones and associated weather conditions. atmospheric disturbances (weather systems) that are
More informationAnnex D. Discharge Modelling Report
Annex D Discharge Modelling Report FINAL REPORT 55 Village Square Drive South Kingstown, RI 02879 Phone: +1 401 789-6224 Fax: +1 401 789-1932 www.asascience.com Oil Spill, Produced Water, Drilling Mud
More informationWinter Storm of 15 December 2005 By Richard H. Grumm National Weather Service Office State College, PA 16803
Winter Storm of 15 December 2005 By Richard H. Grumm National Weather Service Office State College, PA 16803 1. INTRODUCTION A complex winter storm brought snow, sleet, and freezing rain to central Pennsylvania.
More informationTransactions on Ecology and the Environment vol 20, 1998 WIT Press, ISSN
Assessment of the risk of shore contamination by offshore oil spills: model formulation A.N Findikakis*, A.W.K. Lav/ & Y. Papadimitrakis^ ^Bechtel National Inc., San Francisco Email: anfindik@bechtei com
More informationTHE INFLUENCE OF THE METEOROLOGICAL FORCING DATA ON THE RECONSTRUCTIONS OF HISTORICAL STORMS IN THE BLACK SEA
THE INFLUENCE OF THE METEOROLOGICAL FORCING DATA ON THE RECONSTRUCTIONS OF HISTORICAL STORMS IN THE BLACK SEA Vasko Galabov, Anna Kortcheva National Institute of Meteorology and Hydrology- Bulgarian Academy
More informationExamples of Pressure Gradient. Pressure Gradient Force. Chapter 7: Forces and Force Balances. Forces that Affect Atmospheric Motion 2/2/2015
Chapter 7: Forces and Force Balances Forces that Affect Atmospheric Motion Fundamental force - Apparent force - Pressure gradient force Gravitational force Frictional force Centrifugal force Forces that
More informationBoil Model. Back Tracking of Oil Slick Movements in Offshore of Arabian Gulf Marine Waters. Developed By. Khaled Al-Salem April 2013
Boil Model Back Tracking of Oil Slick Movements in Offshore of Arabian Gulf Marine Waters Developed By Khaled Al-Salem April 2013 COASTAL AND AIR POLLUTION DEPARTMENT KUWAIT INSTITUTE FOR SCIENTIFIC RESEARCH
More informationPROJECTION OF FUTURE STORM SURGE DUE TO CLIMATE CHANGE AND ITS UNCERTAINTY A CASE STUDY IN THE TOKYO BAY
Proceedings of the Sixth International Conference on Asian and Pacific Coasts (APAC 2011) December 14 16, 2011, Hong Kong, China PROJECTION OF FUTURE STORM SURGE DUE TO CLIMATE CHANGE AND ITS UNCERTAINTY
More informationA model study of the circulation in the Pearl River Estuary (PRE) and its adjacent coastal waters: 2. Sensitivity experiments
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C5, 3157, doi:10.1029/2002jc001452, 2003 A model study of the circulation in the Pearl River Estuary (PRE) and its adjacent coastal waters: 2. Sensitivity
More informationSimulating the dispersal of aging oil from the Deepwater Horizon spill with a Lagrangian approach
Simulating the dispersal of aging oil from the Deepwater Horizon spill with a Lagrangian approach Elizabeth W. North 1, E. Eric Adams 2, Zachary Schlag 1, Christopher R. Sherwood 3, Rouying He 4, Kyung
More information(April 7, 2010, Wednesday) Tropical Storms & Hurricanes Part 2
Lecture #17 (April 7, 2010, Wednesday) Tropical Storms & Hurricanes Part 2 Hurricane Katrina August 2005 All tropical cyclone tracks (1945-2006). Hurricane Formation While moving westward, tropical disturbances
More informationVOYAGE (PASSAGE) PLANNING
VOYAGE (PASSAGE) PLANNING Introduction O Passage planning or voyage planning is a procedure of developing a complete description of a vessel's voyage from start to finish. O Production of a passage plan
More informationWind Gyres. curl[τ s τ b ]. (1) We choose the simple, linear bottom stress law derived by linear Ekman theory with constant κ v, viz.
Wind Gyres Here we derive the simplest (and oldest; Stommel, 1948) theory to explain western boundary currents like the Gulf Stream, and then discuss the relation of the theory to more realistic gyres.
More informationProjection of Extreme Wave Climate Change under Global Warming
Hydrological Research Letters, 4, 15 19 (2010) Published online in J-STAGE (www.jstage.jst.go.jp/browse/hrl). DOI: 10.3178/HRL.4.15 Projection of Extreme Wave Climate Change under Global Warming Nobuhito
More informationModeling of deep currents in the Japan/East Sea
Modeling of deep currents in the Japan/East Sea Olga Trusenkova V.I.Il ichev Pacific Oceanological Institute, FEB RAS Vladivostok, Russia PICES 2014 Annual Meeting, 16-26 October 2014, Korea, Yeosu Deep
More informationOcean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity?
Name: Date: TEACHER VERSION: Suggested Student Responses Included Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity? Introduction The circulation
More informationCHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS
CHAPTER 9 ATMOSPHERE S PLANETARY CIRCULATION MULTIPLE CHOICE QUESTIONS 1. Viewed from above in the Northern Hemisphere, surface winds about a subtropical high blow a. clockwise and inward. b. counterclockwise.
More informationSMAST Technical Report The Performance of a Coupled 1-D Circulation and Bottom Boundary Layer Model with Surface Wave Forcing
1 SMAST Technical Report 01-03-20 The Performance of a Coupled 1-D Circulation and Bottom Boundary Layer Model with Surface Wave Forcing Y. Fan and W. S. Brown Ocean Process Analysis Laboratory Institute
More informationDRIVEN LARVAL TRANSPORT ON SALEH BAY, SUMBAWA, INDONESIA *)
BAROTROPIC TIDAL AND WIND-DRIVEN DRIVEN LARVAL TRANSPORT ON SALEH BAY, SUMBAWA, INDONESIA *) Widodo S. Pranowo 1), Yulia Herdiani 2) Ivonne M. Radjawane 3) 2), *) Presenting on WOM-12 APEC/MRC/OMISAR in
More informationOceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question.
Oceanography Quiz 2 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The highest and lowest tides are known as the spring tides. When do these occur? a.
More informationOSCILLATIONS OF SEMI-ENCLOSED WATER BODY INDUCED BY HURRICANES. Yuan-Hung Paul Tan 1 and Jiin-Jen Lee 1
OSCILLATIONS OF SEMI-ENCLOSED WATER BODY INDUCED BY HURRICANES Yuan-Hung Paul Tan 1 and Jiin-Jen Lee 1 The primary focus of this research is to study the oscillations of semi-enclosed water body induced
More informationTropical Update. 5 AM EDT Monday, October 8, 2018 Tropical Storm Michael, Tropical Storm Leslie, Invest 92L (10%) & African Tropical Wave (50%)
Tropical Update 5 AM EDT Monday, October 8, 2018 Tropical Storm Michael, Tropical Storm Leslie, Invest 92L (10%) & African Tropical Wave (50%) This update is intended for government and emergency response
More informationESCI 241 Meteorology Lesson 19 Tropical Cyclones Dr. DeCaria
ESCI 241 Meteorology Lesson 19 Tropical Cyclones Dr. DeCaria READING: Chapter 16 GENERAL A tropical cyclone is a large, low-pressure system that forms over the tropical oceans. Tropical cyclones are classified
More information