ROMS modeling of stormwater plumes and anthropogenic nitrogen inputs in the SCB Eileen Idica PhD candidate, Dept Civil &

Slides:

Advertisements

Similar presentations

An atmosphere-ocean coupled regional climate model for the Mediterranean Alberto Elizalde Daniela Jacob Uwe Mikolajewicz Max Planck Institute for Meterology.

Advertisements

Regional and Coastal Circulation Modeling: California Current System Art Miller Scripps Institution of Oceanography ECOFOR Workshop Friday Harbor, WA September.

LARGE EDDY SIMULATION Chin-Hoh Moeng NCAR.

ROMS User Workshop, October 2, 2007, Los Angeles

David J. Sailor1 and Hongli Fan2 1. Portland State University

1 Preliminary Simulation of the Regional Coupled Atmosphere-Ocean Model in the Southern California Coastal Regions (Santa Ana Winds and Air-Sea Interaction)

WHERE IS F3 IN MODELING LARVAL DISPERSAL? Satoshi Mitarai, David Siegel University of California, Santa Barbara, CA Kraig Winters Scripps Institution of.

Concept test We, human beings, along with all animals are causing a net increase of atmospheric CO 2 because our breath contains CO 2 when we exhale. (1)

Seasonal and Interannual Variability of Peruvian anchovy Population Dynamics --progress report-- Yi Xu and Fei Chai June 2007.

Coastal Downscaling: Can CESM fields successfully force regional coastal ocean simulations with strong freshwater forcing? (YES) Parker MacCready (U. of.

NAFE’06 Planning Workshop 1 A BMRC and eWater Perspective Clara Draper Dr. Jeffrey Walker & Dr. Peter Steinle (BMRC)

A Simple Approach to Modeling Iron Limitation of Primary Production in the Gulf of Alaska A Simple Approach to Modeling Iron Limitation of Primary Production.

Chesapeake Bay Lagrangian Floats Analysis. Motivation Lagrangian float has its advantage in describing waters from different origins. We follow definition.

P. N. Vinayachandran Centre for Atmospheric and Oceanic Sciences (CAOS) Indian Institute of Science (IISc) Bangalore Summer.

Bridging the Gap between idealized and realistic numerical river plume simulations Robert Hetland Texas A&M University.

Numerical Simulation of Oceanic Circulation in the Southern California Bight Changming Charles Dong IGPP, UCLA Collaborators: James McWilliams, Meite Blaas,

National Center for Earth-surface Dynamics Modeling physical and ecological dynamics of channel systems that shape Earth’s surface Moving boundary problems.

Iain D. Boyd University of Michigan Modeling of Ion Sputtering and Product Transport.

Flow, Fish and Fishing 2007 All-Hands Meeting. F3’s Bottom Line… Larval transport is a stochastic process driven by coastal stirring Fish stocks, yields.

Coupled physical-biogeochemical modeling of the Louisiana Dead Zone Katja Fennel Dalhousie University Rob Hetland Texas A&M Steve DiMarco.

Connecting the sound to the shelf: a numerical modeling study of estuarine exchange flow in the Salish Sea Dave Sutherland 1 Parker MacCready 1, Neil Banas.

Multiple-scale Variability in the Southern California Bight Oceanic Current System Changming Charles Dong Institute of Geophysical and Planetary Physics,

COLLABORATORS: P. Estrade, S. Herbette, C. Lett, A. Peliz, C. Roy, B. Sow, C. Roy EDDY-DRIVEN DISPERSION IN COASTAL UPWELLING SYSTEMS California Canary.

ROMS Application into Pacific Ocean and US West Coast at JPL Carrie Zhang and the JPL ROMS Group: Yi Chao, Jei Choi, Peggy Li, Zhijin Li, Xiaochun Wang.

Anthropogenic ocean warming: A stress on ocean ecosystems David W. Pierce Tim P. Barnett Climate Research Division Scripps Institution of Oceanography.

Effects of Climate Change on Marine Ecosystems David Mountain US CLIVAR Science Symposium 14 July 2008.

Satellite Data Assimilation into a Suspended Particulate Matter Transport Model.

Effects of Ocean-Atmosphere Coupling in a Modeling Study of Coastal Upwelling in the Area of Orographically-Intensified Flow Natalie Perlin, Eric Skyllingstad,

Oceanic and Atmospheric Modeling of the Big Bend Region Steven L. Morey, Dmitry S. Dukhovksoy, Donald Van Dyke, and Eric P. Chassignet Center for Ocean.

River plume experiments with HYCOM in an idealized basin Rafael Vergara Schiller Villy Kourafalou University of Miami - RSMAS 11 th HYCOM meeting – Apr.

Scientific Approaches to Assess Impacts Associated with Seawater Desalination Susan C. Paulsen, Ph.D., P.E. Vice President and Senior Scientist Desal Conference.

Numerical Simulation of an Upwelling Event in the Southern California Bight (SCB) Changming “Charles” Dong IGPP, UCLA Collaborators: J. McWilliams, M.

SCCOOS Goals and Efforts Within COCMP, SCCOOS aims to develop products and procedures—based on observational data—that effectively evaluate and improve.

Dale haidvogel Nested Modeling Studies on the Northeast U.S. Continental Shelves Dale B. Haidvogel John Wilkin, Katja Fennel, Hernan.

Downscaling Future Climate Scenarios for the North Sea 2006 ROMS/TOMS Workshop, Alcalá de Henares, 6-8 November Bjørn Ådlandsvik Institute of Marine Research.

Estimating and Predicting Ocean Currents in the U.S. coastal oceans John D. Farrara*, Yi Chao, Zhijin Li, Xiaochun Wang*, Hongchun Zhang*, Peggy Li, Quoc.

The Influence of the Indonesian Throughflow on the Eastern Pacific Biogeochimical Conditions Fig.1 The last year of the two runs is used to force offline.

National Consultation with TNMC 3 May 2005, Bangkok WUP-FIN Phase II – Bank erosion study.

IoE The Basics of Satellite Oceanography. 8. Mesoscale variability and coastal pollution Lecture 8 Mesoscale variability and coastal pollution.

Application of ROMS for the Spencer Gulf and on the adjacent shelf of South Australia Carlos Teixeira & SARDI Oceanography Group Aquatic Sciences 2009.

1) What is the variability in eddy currents and the resulting impact on global climate and weather? Resolving meso-scale and sub- meso-scale ocean dynamics.

1. Introduction Boundary-layer clouds are parameterized in general circulation model (GCM), but simulated in Multi-scale Modeling Framework (MMF) and.

Modeling the Gulf of Alaska using the ROMS three-dimensional ocean circulation model Yi Chao 1,2,3, John D. Farrara 2, Zhijin Li 1,2, Xiaochun Wang 2,

Modeling transport and deposition of the Mekong River sediment Z. George Xue 1 * Ruoying He 1, J.Paul Liu 1, John C Warner 2 1.Dept. of Marine, Earth and.

Filling the Gap: The Structure of Near Coastal Winds Jeroen Molemaker, Francois Colas and Xavier Capet University of California Los Angeles.

Southern California Coast Observed Temperature Anomalies Observed Salinity Anomalies Geostrophic Along-shore Currents Warming Trend Low Frequency Salinity.

Wind-SST Coupling in the Coastal Upwelling --- An Empirical Numerical Simulation X. Jin, C. Dong, and J. C. McWilliams (IGPP/UCLA) D. B. Chelton (COAS/OSU)

Coastal Oceanography Outline Global coastal ocean Dynamics Western boundary current systems Eastern boundary current systems Polar ocean boundaries Semi-enclosed.

On the role of eddies for coastal productivity and carbon cycling Hartmut Frenzel 1, Nicolas Gruber 2,1, Gian-Kasper Plattner 2, Takeyoshi Nagai 3,1, James.

OCEANS INTRO AND ESTUARY REVIEW Module 7. THE OCEAN IS A DYNAMIC SYSTEM- ALWAYS CHANGING!  The ocean is an important source of food and mineral resources.

Dmitry Dukhovskoy, Andrey Proshutinsky and Mary-Louise Timmermans Center for Ocean-Atmospheric Prediction Studies Florida State University Acknowledgement:

THE BC SHELF ROMS MODEL THE BC SHELF ROMS MODEL Diane Masson, Isaak Fain, Mike Foreman Institute of Ocean Sciences Fisheries and Oceans, Canada The Canadian.

Inter-annual Simulation with the South Florida HYCOM Nested Model Roland Balotro, Villy Kourafalou and Alan Wallcraft 2005 Layered Ocean Model User’s Workshop.

1 Modeling and Forecasting for SCCOOS (Southern California Coastal Ocean Observing System) Yi Chao 1, 2 & Jim McWilliams 2 1 Jet Propulsion Laboratory,

I NCORPORATION OF C ONTINENTAL AND U RBAN R UN - OFF INTO A C OASTAL C IRCULATION M ODEL : A PPLICATION TO THE C ATALAN C OAST M. L ISTE, M. G RIFOLL,

Coupling ROMS and CSIM in the Okhotsk Sea Rebecca Zanzig University of Washington November 7, 2006.

Earth Science SAGE Workbook SAGE Review

Coupled atmosphere-ocean simulation on hurricane forecast

Shelf-basin exchange in the Western Arctic Ocean

UCLA Regional Earth System Modeling for VOCALS

COSA Committee Meeting

Studying Hector: meteorology and tracer transport

Monitoring and Research:

Global Simulation of CH3Cl

Investigating Dansgaard-Oeschger events via a 2-D ocean model

Andreas Münchow, College of Marine Studies, University of Delaware

66-SE-CMEMS-CALL2: Lot-3 Benefits of dynamically modelled river discharge input for ocean and coupled atmosphere-land-ocean systems Hao Zuo, Fredrik Wetterhall,

Adjoint Sensitivity Studies on the US East Coast

SUB-TIDAL VARIABILITY IN THE HUDSON RIVER PLUME AS A RESULT OF HIGH FREQUENCY FORCING #543 Hunter, E.J., Rutgers University, Chant, R.J., Rutgers University,

Presentation transcript:

ROMS modeling of stormwater plumes and anthropogenic nitrogen inputs in the SCB Eileen Idica PhD candidate, Dept Civil & Env Engineering, UCLA Advisor: Keith Stolzenbach Regional Oceanic Modeling System (ROMS) SCB Configuration 1 km horizontal resolution 40 vertical levels surface forcings ◦ momentum (MM5) ◦ freshwater and heat fluxes lateral boundary fluxes from larger US West Coast ROMS solution anticipated to have hourly solutions

Analytical, one-day storm event 500 cms daily mean flow Salinity of discharge is zero Passive tracer released with discharge Half-Gaussian vertical input profile Example: Los Angeles River stormwater discharge simulation Would like to determine plume dynamics within a range of ocean forcings model suspended sediments, settling, and sorption in stormwater discharge investigate relative space and time scales in which these processes affect transport of contaminants carried by the stormwater plume

Impact of anthropogenic nitrogen to the Southern California Bight Use ROMS and ecosystem model to simulate: i) low upwelling year ( ) ii)high upwelling year ( ) i) only upwelled nitrogen ii) “natural” land input of nitrogen iii) existing stormwater and wastewater inputs (18 major rivers, 4 largest treatment facilities) ROMS ecosystem model (Gruber et al. 2006) What, if any, biological “signal” will we observe in the set of simulations from anthropogenic inputs, and on what spatial and time scales?