Coastal Inlets and Tidal Basins
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Modeling Dynamic Processes of Mondego Estuary and Óbidos Lagoon Using Delft3d
Journal of Marine Science and Engineering Article Modeling Dynamic Processes of Mondego Estuary and Óbidos Lagoon Using Delft3D Joana Mendes , Rui Ruela, Ana Picado, João Pedro Pinheiro, Américo Soares Ribeiro , Humberto Pereira and João Miguel Dias * Physics Department, CESAM–Centre for Environmental and Marine Studies, University of Aveiro, 3810-193 Aveiro, Portugal; [email protected] (J.M.); [email protected] (R.R.); [email protected] (A.P.); [email protected] (J.P.P.); [email protected] (A.S.R.); [email protected] (H.P.) * Correspondence: [email protected] Abstract: Estuarine systems currently face increasing pressure due to population growth, rapid economic development, and the effect of climate change, which threatens the deterioration of their water quality. This study uses an open-source model of high transferability (Delft3D), to investigate the physics and water quality dynamics, spatial variability, and interrelation of two estuarine systems of the Portuguese west coast: Mondego Estuary and Óbidos Lagoon. In this context, the Delft3D was successfully implemented and validated for both systems through model-observation comparisons and further explored using realistically forced and process-oriented experiments. Model results show (1) high accuracy to predict the local hydrodynamics and fair accuracy to predict the transport and water quality of both systems; (2) the importance of the local geomorphology and estuary dimensions in the tidal propagation and asymmetry; (3) Mondego Estuary (except for the south arm) has a higher water volume exchange with the adjacent ocean when compared to Óbidos Lagoon, resulting from the highest fluvial discharge that contributes to a better water renewal; (4) the dissolved oxygen (DO) varies with water temperature and salinity differently for both systems. -
Analysis of Tidal Prism Evolution and Characteristics of the Lingdingyang
MATEC Web of Conferences 25, 001 0 6 (2015) DOI: 10.1051/matecconf/201525001 0 6 C Owned by the authors, published by EDP Sciences, 2015 Analysis of Tidal Prism Evolution and Characteristics of the Lingdingyang Bay at Pearl River Estuary Shenguang Fang, Yufeng Xie & Liqin Cui Key laboratory of the Pearl River Estuarine Dynamics and Associated Process Regulation, Ministry of Water Resources, Guangzhou, Guangdong, China ABSTRACT: Tidal prism is a rather sensitive factor of the estuarine ecological environment. The historical evolution of the Lingdingyang water area and its shoreline were analyzed. By using remote sensing data, the evolution of the water area of the bay was also calculated in the past 30 years. Due to reclamation, the water area was greatly decreased during that period, and the most serious decrease occurred between 1988 and 1995. Through establishing the two-dimensional mathematical model of the Pearl River estuary, the tidal prism of the Lingdingyang bay has been calculated and analyzed. The hybrid finite analytic method of fully implicit scheme was adopted in the mathematical model’s dispersion and calculation. The results were verified though the method of combining the field hydrographic data and empirical formula calculation. The results showed that the main tidal entrance of the bay is the Lingdingyang entrance, which accounts for about 87.7% of the total tidal prism, while Hong Kong’s Anshidun waterway accounts for only 12.3% or so. Combining the numerical simulations and the historical evolution analysis of the water area and tidal prism, and compared with that in 1978, it showed that the tidal prism of the bay was greatly decreased, and the reduced area was mainly the inner Lingdingyang bay, which accounted for 88.4% of the whole shrunken areas. -
Tidal Resonance in the Gulf of Thailand
Ocean Sci., 15, 321–331, 2019 https://doi.org/10.5194/os-15-321-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Tidal resonance in the Gulf of Thailand Xinmei Cui1,2, Guohong Fang1,2, and Di Wu1,2 1First Institute of Oceanography, Ministry of Natural Resources, Qingdao, 266061, China 2Laboratory for Regional Oceanography and Numerical Modelling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266237, China Correspondence: Guohong Fang (fanggh@fio.org.cn) Received: 12 August 2018 – Discussion started: 24 August 2018 Revised: 1 February 2019 – Accepted: 18 February 2019 – Published: 29 March 2019 Abstract. The Gulf of Thailand is dominated by diurnal 1323 m. If the GOT is excluded, the mean depth of the rest tides, which might be taken to indicate that the resonant fre- of the SCS (herein called the SCS body and abbreviated as quency of the gulf is close to one cycle per day. However, SCSB) is 1457 m. Tidal waves propagate into the SCS from when applied to the gulf, the classic quarter-wavelength res- the Pacific Ocean through the Luzon Strait (LS) and mainly onance theory fails to yield a diurnal resonant frequency. In propagate in the southwest direction towards the Karimata this study, we first perform a series of numerical experiments Strait, with two branches that propagate northwestward and showing that the gulf has a strong response near one cycle per enter the Gulf of Tonkin and the GOT. The energy fluxes day and that the resonance of the South China Sea main area through the Mindoro and Balabac straits are negligible (Fang has a critical impact on the resonance of the gulf. -
Coastal Squeeze Evidence and Monitoring Requirement Review
Coastal Squeeze Evidence and Monitoring Requirement Review Oaten, J., Brooks, A. and Frost, N. ABPmer NRW Evidence Report No. 307 Date www.naturalresourceswales.gov.uk About Natural Resources Wales Natural Resources Wales’ purpose is to pursue sustainable management of natural resources. This means looking after air, land, water, wildlife, plants and soil to improve Wales’ well-being, and provide a better future for everyone. Evidence at Natural Resources Wales Natural Resources Wales is an evidence based organisation. We seek to ensure that our strategy, decisions, operations and advice to Welsh Government and others are underpinned by sound and quality-assured evidence. We recognise that it is critically important to have a good understanding of our changing environment. We will realise this vision by: Maintaining and developing the technical specialist skills of our staff; Securing our data and information; Having a well resourced proactive programme of evidence work; Continuing to review and add to our evidence to ensure it is fit for the challenges facing us; and Communicating our evidence in an open and transparent way. This Evidence Report series serves as a record of work carried out or commissioned by Natural Resources Wales. It also helps us to share and promote use of our evidence by others and develop future collaborations. However, the views and recommendations presented in this report are not necessarily those of NRW and should, therefore, not be attributed to NRW. www.naturalresourceswales.gov.uk Page 1 Report series: NRW Evidence Report Report number: 307 Publication date: November 2018 Contract number: WAO000E/000A/1174A - CE0529 Contractor: ABPmer Contract Manager: Park, R. -
Estuarine Tidal Response to Sea Level Rise: the Significance of Entrance Restriction
Estuarine, Coastal and Shelf Science 244 (2020) 106941 Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: http://www.elsevier.com/locate/ecss Estuarine tidal response to sea level rise: The significance of entrance restriction Danial Khojasteh a,*, Steve Hottinger a,b, Stefan Felder a, Giovanni De Cesare b, Valentin Heimhuber a, David J. Hanslow c, William Glamore a a Water Research Laboratory, School of Civil and Environmental Engineering, UNSW, Sydney, NSW, Australia b Platform of Hydraulic Constructions (PL-LCH), Ecole Polytechnique F´ed´erale de Lausanne (EPFL), Lausanne, Switzerland c Science, Economics and Insights Division, Department of Planning, Industry and Environment, NSW Government, Locked Bag 1002 Dangar, NSW 2309, Australia ARTICLE INFO ABSTRACT Keywords: Estuarine environments, as dynamic low-lying transition zones between rivers and the open sea, are vulnerable Estuarine hydrodynamics to sea level rise (SLR). To evaluate the potential impacts of SLR on estuarine responses, it is necessary to examine Tidal asymmetry the altered tidal dynamics, including changes in tidal amplification, dampening, reflection (resonance), and Resonance deformation. Moving beyond commonly used static approaches, this study uses a large ensemble of idealised Idealised method estuarine hydrodynamic models to analyse changes in tidal range, tidal prism, phase lag, tidal current velocity, Ensemble modelling Cluster analysis and tidal asymmetry of restricted estuaries of varying size, entrance configuration and tidal forcing as well as three SLR scenarios. For the first time in estuarine SLR studies, data analysis and clustering approaches were employed to determine the key variables governing estuarine hydrodynamics under SLR. The results indicate that the hydrodynamics of restricted estuaries examined in this study are primarily governed by tidal forcing at the entrance and the estuarine length. -
NS-TAST-GD-013 Annex 3 Reference Paper: Analysis of Coastal Flood
ONR Expert Panel on Natural Hazards NS-TAST-GD-013 Annex 3 Reference Paper: Analysis of Coastal Flood Hazards for Nuclear Sites Expert Panel Paper No: GEN-MCFH-EP-2017-2 Sub-Panel on Meteorological & Coastal Flood Hazards October 2018 For more information contact: Office for Nuclear Regulation Building 4, Redgrave Court Merton Road Bootle L20 7HS Email: [email protected] GEN-MCFH-EP-2017-2 TRIM Ref: 2018/316283 Page 1 TABLE OF CONTENTS LIST OF ABBREVIATIONS .......................................................................................................... 3 ACKNOWLEDGEMENTS ............................................................................................................. 4 1 INTRODUCTION ..................................................................................................................... 5 2 OVERVIEW OF COASTAL FLOODING, INCLUDING EROSION AND TSUNAMI IN THE UK ........................................................................................................................................... 6 2.1 Mean sea level ............................................................................................................... 7 2.2 Vertical land movement and gravitational effects ........................................................... 7 2.3 Storm surges ..................................................................................................................8 2.4 Waves ............................................................................................................................ -
Oceanic Tides
International Hydrographie Review, Monaco, LV (2), July 1978 OCEANIC TIDES by Dr. D.E. CARTWRIGHT Institute of Oceanographic Sciences, Bidston, Birkenhead, England This paper was first published in Reports on Progress in Physics, 1977 (40), and is reproduced with the kind permission of the Institute of Physics, London, who retain the copyright. ABSTRACT Tidal research has had a long history, but the outstanding problems still defeat current research techniques, including large-scale computation. The definition of the tide-generating potential, basic to all research, is reviewed in modern terms. Modern usage in analysis introduces the concept of tidal ‘ admittance ’ functions, though limited to rather narrow frequency bands. A ‘ radiational potential ’ has also been found useful in defining the parts of tidal signals which are due directly or indirectly to solar radiation. Laplace’s tidal equations ( l t e ) omit several terms from the full dyna mical equations, including the vertical acceleration. Controversies about the justification for l t e have been fairly well settled by M tt.e s ’ (1974) demonstration that, when regarded as the lowest order internal wave mode in a stratified fluid, solutions of the full equations do converge to those of l t e . Solutions in basins of simple geometry are reviewed and distinguished from attempts, mainly by P r o u d m a n , to solve for the real oceans by division into elementary strips, and from localized syntheses as Used by M u n k for the tides off California. The modern computer seemed to provide a ‘ breakthrough ’ in solving l t e for the world’s oceans, but the results of independent workers differ, mostly because of the inadequacy in their treatment of friction and for the elastic yielding of the Earth. -
Understanding the Relationship Between Sedimentation, Vegetation and Topography in the Tijuana River Estuary, San Diego, CA
University of San Diego Digital USD Theses Theses and Dissertations Spring 5-25-2019 Understanding the relationship between sedimentation, vegetation and topography in the Tijuana River Estuary, San Diego, CA. Darbi Berry University of San Diego Follow this and additional works at: https://digital.sandiego.edu/theses Part of the Environmental Indicators and Impact Assessment Commons, Geomorphology Commons, and the Sedimentology Commons Digital USD Citation Berry, Darbi, "Understanding the relationship between sedimentation, vegetation and topography in the Tijuana River Estuary, San Diego, CA." (2019). Theses. 37. https://digital.sandiego.edu/theses/37 This Thesis: Open Access is brought to you for free and open access by the Theses and Dissertations at Digital USD. It has been accepted for inclusion in Theses by an authorized administrator of Digital USD. For more information, please contact [email protected]. UNIVERSITY OF SAN DIEGO San Diego Understanding the relationship between sedimentation, vegetation and topography in the Tijuana River Estuary, San Diego, CA. A thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Environmental and Ocean Sciences by Darbi R. Berry Thesis Committee Suzanne C. Walther, Ph.D., Chair Zhi-Yong Yin, Ph.D. Jeff Crooks, Ph.D. 2019 i Copyright 2019 Darbi R. Berry iii ACKNOWLEGDMENTS As with every important journey, this is one that was not completed without the support, encouragement and love from many other around me. First and foremost, I would like to thank my thesis chair, Dr. Suzanne Walther, for her dedication, insight and guidance throughout this process. Science does not always go as planned, and I am grateful for her leading an example for me to “roll with the punches” and still end up with a product and skillset I am proud of. -
Assessment of Shelf Sea Tides and Tidal Mixing Fronts in a Global Ocean Model T ⁎ Patrick G
Ocean Modelling 136 (2019) 66–84 Contents lists available at ScienceDirect Ocean Modelling journal homepage: www.elsevier.com/locate/ocemod Assessment of shelf sea tides and tidal mixing fronts in a global ocean model T ⁎ Patrick G. Timkoa,b, , Brian K. Arbicb,c, Patrick Hyderd, James G. Richmane, Luis Zamudioe, Enda O'Dead, Alan J. Wallcrafte, Jay F. Shriverf a Welsh Local Centre, Royal Meteorological Society, UK b Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI, USA c Currently on sabbatical at Institut des Géosciences de L'Environnement (IGE), Grenoble, France, and Laboratoire des Etudes en Géophysique et Océanographie Spatiale (LEGOS), Toulouse, France d UK Met Office, Exeter, UK e Center for Ocean – Atmospheric Prediction Studies, Florida State University, Florida, USA f Naval Research Laboratory, Stennis Space Center, MS, USA ABSTRACT Tidal mixing fronts, which represent boundaries between stratified and tidally mixed waters, are locations of enhanced biological activity. They occur insummer shelf seas when, in the presence of strong tidal currents, mixing due to bottom friction balances buoyancy production due to seasonal heat flux. In this paper we examine the occurrence and fidelity of tidal mixing fronts in shelf seas generated within a global 3-dimensional simulation of the HYbrid Coordinate OceanModel (HYCOM) that is simultaneously forced by atmospheric fields and the astronomical tidal potential. We perform a first order assessment of shelf sea tidesinglobal HYCOM through comparison of sea surface temperature, sea surface tidal elevations, and tidal currents with observations. HYCOM was tuned to minimize errors in M2 sea surface heights in deep water. -
Tidal Datums and Their Applications
U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Ocean Service Center for Operational Oceanographic Products and Services TIDAL DATUMS AND THEIR APPLICATIONS NOAA Special Publication NOS CO-OPS 1 NOAA Special Publication NOS CO-OPS 1 TIDAL DATUMS AND THEIR APPLICATIONS Silver Spring, Maryland June 2000 noaa National Oceanic and Atmospheric Administration U.S. DEPARTMENT OF COMMERCE National Ocean Service Center for Operational Oceanographic Products and Services Center for Operational Oceanographic Products and Services National Ocean Service National Oceanic and Atmospheric Administration U.S. Department of Commerce The National Ocean Service (NOS) Center for Operational Oceanographic Products and Services (CO-OPS) collects and distributes observations and predictions of water levels and currents to ensure safe, efficient and environmentally sound maritime commerce. The Center provides the set of water level and coastal current products required to support NOS’ Strategic Plan mission requirements, and to assist in providing operational oceanographic data/products required by NOAA’s other Strategic Plan themes. For example, CO-OPS provides data and products required by the National Weather Service to meet its flood and tsunami warning responsibilities. The Center manages the National Water Level Observation Network (NWLON) and a national network of Physical Oceanographic Real-Time Systems (PORTSTM) in major U.S. harbors. The Center: establishes standards for the collection and processing of water level and current data; collects and documents user requirements which serve as the foundation for all resulting program activities; designs new and/or improved oceanographic observing systems; designs software to improve CO-OPS’ data processing capabilities; maintains and operates oceanographic observing systems; performs operational data analysis/quality control; and produces/disseminates oceanographic products. -
Coupling of Sea Level Rise, Tidal Amplification, and Inundation
MAY 2014 H O L L E M A N A N D S T A C E Y 1439 Coupling of Sea Level Rise, Tidal Amplification, and Inundation RUSTY C. HOLLEMAN* AND MARK T. STACEY Department of Civil and Environmental Engineering, University of California, Berkeley, Berkeley, California (Manuscript received 1 October 2013, in final form 13 January 2014) ABSTRACT With the global sea level rising, it is imperative to quantify how the dynamics of tidal estuaries and em- bayments will respond to increased depth and newly inundated perimeter regions. With increased depth comes a decrease in frictional effects in the basin interior and altered tidal amplification. Inundation due to higher sea level also causes an increase in planform area, tidal prism, and frictional effects in the newly inundated areas. To investigate the coupling between ocean forcing, tidal dynamics, and inundation, the authors employ a high-resolution hydrodynamic model of San Francisco Bay, California, comprising two basins with distinct tidal characteristics. Multiple shoreline scenarios are simulated, ranging from a leveed scenario, in which tidal flows are limited to present-day shorelines, to a simulation in which all topography is allowed to flood. Simulating increased mean sea level, while preserving original shorelines, produces addi- tional tidal amplification. However, flooding of adjacent low-lying areas introduces frictional, intertidal re- gions that serve as energy sinks for the incident tidal wave. Net tidal amplification in most areas is predicted to be lower in the sea level rise scenarios. Tidal dynamics show a shift to a more progressive wave, dissipative environment with perimeter sloughs becoming major energy sinks. -
Indian River Inlet: an Evaluation by the Committee Cm Tidal Hydraulics
I I July 1994 I o it~ol [m] us Army corps of Engineers Indian River inlet: An Evaluation by the Committee cm Tidal Hydraulics by The Committee on Tidal Hydraulics Approved For Public Release; Distribution Is Unlimited I I I Prepared for Headquarters, U.S. Army Corps of Engineers , ..: PRESENT lvl&BERSEilP OF : ;r .; COMMl~”EE ON ilbAL HYDRAULlb ., ,,.,.: . .; 4’ Members : U ~ ~ L . / ,, .: ‘: ,. F. A. Herrmann,. Jr., Chairman :~Waterways~Experiment Station ‘.: W. H. McAnally,’Jr., Waterways Experiment Station Executive Secretary ., .: L. C. Blake ~ ~Charleston District ~ H. L. Butler ~ .kVaterwaysiExperiment Station j .’ A. J. Combe j New Orleans District ~ :, .. Dr. J. Harrison ., ,Waterways ‘.Experimen~ Station Dr. B. W. Holliday :-leadquarters~ U.S. Army Corps of : Engineers ~ . ‘, ;. J. Merino ~ South Pacific :Division ., V. R. Pankow : Water Resources Support Center E. A. Reindl, Jr. j Galveston tiistrict . A. D. Schuldt ~ Seattle Dist~ct !. R. G. Vann ~ Norfolk District ,. C. J. Wener ‘: New England Division - ,, /. Liaison S. B. Powell He,adquarters,., U.S. Army Corps of VEngineers” : , ., ,. Consultants Dr. R. B. Krone - Davis, CA Dr. D. W. Pritchard Severna Park,” MD H. B. Simmons “’ Vicksburg, MS” Corresponding Member C. F. Wicker ; We~stChester, PA ~ :. Destroy this report when no longer needed.. Do not return it to the originator. July 1994 1 Indian River Inlet: An Evaluation I by the Committee on Tidal Hydraulics by The Committee on Ttdal Hydraulics Final report Approvedforpublicrelease; distributionis unlimited Prepared for U.S. Army Corps of Engineers Washington, DC 20314-6199 Published by U.S. Army Corps of Engineers Waterways Experiment Station 3909 Halls Ferry Road Vicksburg, MS 39180-6199 WaterwaysExperiment StatIonCataloging-in-PublicatlqnData I United States.