Jerry D. Wiggert (USM) Wen Long (UMCES) Jiangtao Xu (NOAA/NOS/CSDL) Raleigh R. Hood (UMCES) Erin B. Jones (USM) Lyon W. J. Lanerolle (NOAA) Christopher.

Slides:



Advertisements
Similar presentations
Geographical Information System & Modelling LIFE02/ENV/P/
Advertisements

Workshop Steering Committee: Carl Cerco Carl Friedrichs (STAC) Marjy Friedrichs (STAC) Raleigh Hood David Jasinski Wen Long Kevin Sellner (STAC) Time:
Skill Assessment of Multiple Hypoxia Models in the Chesapeake Bay and Implications for Management Decisions Isaac (Ike) Irby - Virginia Institute of Marine.
The ChesROMS Community Model
Evaluating Models for Chesapeake Bay Dissolved Oxygen: Helping Carl Friedrichs Virginia Institute of Marine Science Gloucester Point, Virginia, USA Presented.
WP12. Hindcast and scenario studies on coastal-shelf climate and ecosystem variability and change Why? (in addition to the call text) Need to relate “today’s”
Physical Oceanographic Observations and Models in Support of the WFS HyCODE College of Marine Science University of South Florida St. Petersburg, FL HyCode.
A Simple Model for Oxygen Dynamics in Chesapeake Bay Malcolm Scully 1)Background and Motivation 2)Simplified Modeling Approach 3)Importance of Physical.
Coupled physical-biogeochemical modeling of the Louisiana Dead Zone Katja Fennel Dalhousie University Rob Hetland Texas A&M Steve DiMarco.
US IOOS Modeling Testbed Leadership Teleconference May 3, 2011 Estuarine Hypoxia Team Carl Friedrichs, VIMS
The Physical Modulation of Seasonal Hypoxia in Chesapeake Bay Malcolm Scully Outline: 1)Background and Motivation 2)Role of Physical Forcing 3)Simplified.
A Super-Regional Modeling Testbed for Improving Forecasts of Environmental Processes for the U.S. Atlantic and Gulf of Mexico Coasts Cyberinfrastructure.
Combining Observations & Numerical Model Results to Improve Estimates of Hypoxic Volume within the Chesapeake Bay JGR-Oceans, October 2013 issue Aaron.
A Super-Regional Modeling Testbed for Improving Forecasts of Environmental Processes for the U.S. Atlantic and Gulf of Mexico Coasts Don Wright, SURA Principal.
1 Using Multi-temporal MODIS 250 m Data to Calibrate and Validate a Sediment Transport Model for Environmental Monitoring of Coastal Waters.
Comparing observed and modeled estimates of hypoxic volume within the Chesapeake Bay, USA, to improve the observational sampling strategy Aaron J. Bever.
Transitioning a Chesapeake Bay Ecological Prediction System to Operations January 24, 2012 D. Green 1, C. Brown 1, F. Aikman 1, A. Siebers 1, H. Tolman.
DeZoZoo Investigators Meeting 5 December What are we doing here today? What we said we would do. What we actually did. What does it mean. What and.
A T HREE- D IMENSIONAL W ATER Q UALITY M ODEL OF S OUTHERN P UGET S OUND Greg Pelletier, P.E., Mindy Roberts, P.E., Skip Albertson, P.E., and Jan Newton,
Bathymetry Controls on the Location of Hypoxia Facilitate Possible Real-time Hypoxic Volume Monitoring in the Chesapeake Bay Aaron J. Bever 1, Marjorie.
Isaac (Ike) Irby 1, Marjorie Friedrichs 1, Yang Feng 1, Raleigh Hood 2, Jeremy Testa 2, Carl Friedrichs 1 1 Virginia Institute of Marine Science, The College.
Isaac (Ike) Irby 1, Marjorie Friedrichs 1, Yang Feng 1, Raleigh Hood 2, Jeremy Testa 2, Carl Friedrichs 1 1 Virginia Institute of Marine Science, The College.
1 NOS Coastal Ocean Operational Forecast Systems Presented By: Patrick Burke (NOS/CO-OPS) Contributors: Aijun Zhang (CO-OPS), Peter Stone (CO-OPS), Edward.
Fig. 4. Target diagram showing how well the total 3D HV from each model is reproduced by different stations sets. Sets correspond to; min10: 10 stations.
Year 3 Research and Priorities Jeremy Testa Horn Point Laboratory December 9, 2008 Primary Scientific Question What C sources are missing from the Bay.
Courtney K. Harris Virginia Institute of Marine Sciences In collaboration with Katja Fennel and Robin Wilson (Dalhousie), Rob Hetland (TAMU), Kevin Xu.
Gulf of Maine / Scituate Harbor - Extratropical Domain Shelf Hypoxia ChesROMS Long & Hood UMCES Estuarine Hypoxia Inundation Cyber Infrastructure IOOS.
Modeling Support for James River Chlorophyll Study Dave Jasinski, CEC Jim Fitzpatrick, HDR|HrydroQual Andrew Parker, Tetra Tech Harry Wang, VIMS Presentation.
A Super-Regional Modeling Testbed for Improving Forecasts of Environmental Processes for the U.S. Atlantic and Gulf of Mexico Coasts Don Wright, SURA Principal.
Super-Regional Testbed to Improve Models of Environmental Processes on the U.S. Atlantic and Gulf of Mexico Coasts Shelf Hypoxia Progress/ Plans John Harding.
Super-Regional Modeling Testbed to Improve Forecasts of Environmental Processes for the U.S. Atlantic and Gulf of Mexico Coasts Wright, L.D.; Signell,
DEAD ZONE Hypoxic Zone in the Gulf of Mexico. What is it? The hypoxic zone in the northern Gulf of Mexico refers to an area along the Louisiana- Texas.
Office of Coast Survey / Coast Survey Development Lab Transition, Progress, Challenges and Future Directions Richard Patchen NOAA’S National Ocean Service.
Is there any air down there? Using multiple 3D numerical models to investigate hypoxic volumes within the Chesapeake Bay, USA Aaron J. Bever 1, Marjorie.
Combining Observations & Models to Improve Estimates of Chesapeake Bay Hypoxic Volume* Aaron Bever, Marjorie Friedrichs, Carl Friedrichs, Malcolm Scully,
Anoxia in Narragansett Bay Can we predict it?.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Hydrologic and Water Quality Modeling of the Chesapeake Bay Watershed Huan.
NOAA/NOS/OCS/Coast Survey Development Laboratory Lyon Lanerolle 1,2, Richard Patchen 1 and Frank Aikman III 1 1 National Oceanic and Atmospheric Administration.
US IOOS Modeling Testbed Leadership Teleconference May 3, 2011 Estuarine Hypoxia Team Carl Friedrichs, VIMS
Evaluating Models of Chesapeake Bay Low Oxygen Dead Zones: Helping Federal Agencies Improve Water Quality Carl Friedrichs Virginia Institute of Marine.
COMT Project meeting Ecological Forecasting, Existing status of CBEPS (Chesapeake Bay Ecological Prediction System), Future developments of CBEPS, Plan.
A GLOBAL PERSPECTIVE ON THE LINKAGE BETWEEN EUTROPHICATION AND HYPOXIA Robert Diaz College of William and Mary Virginia Institute of Marine Science
U.S. Eastern Continental Shelf Carbon Budget: Modeling, Data Assimilation, and Analysis U.S. ECoS Science Team* ABSTRACT. The U.S. Eastern Continental.
U.S. ECoS U.S. Eastern Continental Shelf Carbon Budget: Modeling, Data Assimilation, and Analysis A project of the NASA Earth System Enterprise Interdisciplinary.
ROMS hydrodynamic model ROMS-RCA model for hypoxia prediction RCA biogeochemical model Model forced by NARR/WRF meteorological forcing, river discharge.
Office of Coast Survey / CSDL Sensitivity Analysis of Temperature and Salinity from a Suite of Numerical Ocean Models for the Chesapeake Bay Lyon Lanerolle.
This project is supported by the NASA Interdisciplinary Science Program The Estuarine Hypoxia Component of the Coastal Ocean Modeling Testbed: Providing.
Transitioning a Chesapeake Bay Ecological Prediction System to Operations 1. Introduction NOAA’s National Weather Service (NWS) Draft Strategic Plan (22.
Puget Sound Oceanography 2009 Course overview. Geology of Puget Sound Started from Pangaea Plate movement, subduction zones, volcanoes and valleys Glaciation.
Results of the US IOOS Testbed for Comparison of Hydrodynamic and Hypoxia Models of Chesapeake Bay Carl Friedrichs (VIMS) and the Estuarine Hypoxia Team.
Super-Regional Modeling Testbed Estuarine Hypoxia Team Carl Friedrichs (VIMS) – Team Leader Federal partners David Green (NOAA-NWS) – Transition to operations.
Development of the Neuse Estuary Eutrophication Model: Background and Calibration By James D. Bowen UNC Charlotte.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Satellite Observation and Model Simulation of Water Turbidity in the Chesapeake.
NOAA Chesapeake Bay Office Fisheries Ecosystem Modeling Efforts Howard Townsend, Hongguang Ma, and Maddy Sigrist NOAA Chesapeake Bay Office National Ecosystem.
with contributions from:
The Installation of ChesROMS1.1 Wen Long Jiangtao Xu Lyon W.J. Lanerolle Jerry D. Wiggert David Potsiadlo Kyle Wilcox Thomas F. Gross Raleigh R. Hood Raghu.
Estuarine Hypoxia Component of Testbed 2 Marjorie Friedrichs, VIMS, lead Carl Friedrichs, VIMS, co-lead Wen Long and Raleigh Hood, UMCES Malcolm Scully,
U.S. IOOS Testbed Comparisons: Hydrodynamics and Hypoxia Marjy Friedrichs Virginia Institute of Marine Science Including contributions from the entire.
Regional Advanced School on Physical and Mathematical Tools for the study of Marine Processes of Coastal Areas Physical and Biogeochemical Coupled Modelling.
Abstract Man-made dams influence more than just the flow of water in a river. The build up of sediments and organic matter, increased residence times,
US IOOS Modeling Testbed Leadership Teleconference May 3, 2011 Shelf Hypoxia John Harding, Northern Gulf Institute
Eutrophication, Hypoxia, and Ocean Acidification Puget Sound Oceanography 2011.
1/15 Place Photo Here Biophysical Modeling Mark Rowe Ecosystem Dynamics University of Michigan, CILER.
FIGURE 17.1 A simple nitrogen and water balance for ‘‘Dave the Sea Lion.’’ Both nitrogen and water flows are in units of grams per 40 days. See text for.
Modeling phytoplankton seasonal variation and nutrients budget of a Semi-Arid region ecosystem in the Southern Mediterranean Sea: -Case of the Bizerte.
Hypoxia Forecasts as a Tool for Chesapeake Bay Fisheries
Estuarine Hypoxia Component of Testbed 2
AquaSpace Case Study Great Bay Piscataqua and Long Island Sound, USA: Issues and Tools The research leading to these results has been undertaken as part.
D. Green1, C. Brown1, F. Aikman1, A. Siebers1, H. Tolman1, M. Ji1, D
Presentation transcript:

Jerry D. Wiggert (USM) Wen Long (UMCES) Jiangtao Xu (NOAA/NOS/CSDL) Raleigh R. Hood (UMCES) Erin B. Jones (USM) Lyon W. J. Lanerolle (NOAA) Christopher W. Brown (CICS-ESSIC NOAA) This research funded by NOAA-MERHAB & IOOS-SURA Application of a Coupled Physical-Biogeochemical Model to Simulate and Forecast the Ecological Variability of Chesapeake Bay

Aquatic Sciences, 20 February 2013 Outline - ChesROMS Community Model - Biogeochemical Model Implementation & Waypoints - Assessment of Ecosystem Model Solutions - Concluding Remarks MODIS Image from Kemp et al. 2005

Aquatic Sciences, 20 February 2013 ChesROMS Community Model ✦ ROMS 3.0 ✦ Curvilinear Horizontally ✦ σ-coordinate Vertically ✦ Includes major tributaries ✦ Coarse mesh for model development (100*150*20) ✦ Forcing: Tides, Winds, Heat Fluxes and Rivers ✦ Validated Physical Model w/ 15-Year Hindcast (Xu et al., accepted) ✦ Currently expanding the biogeochemical model ✦ Goal: Improved Simulation of BGC processes & Water Quality Fields ✦ Use Output to inform Ecological Models (HABs, pathogens, etc.) ✦ Open Source Available at: ChesROMS Team: Chris Brown, Tom Gross, Brooke Denton, Raleigh Hood, Mohan Karyampudi, Lyon Lanerolle, Wen Long, Raghu Murtugudde, Dave Potsiadlo, M. Bala Krishna Prasad, Jerry Wiggert, Jiangtao Xu

Aquatic Sciences, 20 February 2013 CBP Sampling Sites CB4.1C (upper bay) CB5.3 (middle bay) CB6.3 (lower bay) Map Courtesy of Chesapeake Bay Program Chesapeake Bay Program ( Data Used For: Initial Conditions River Boundary Conditions Solution Validation Sites (following Xu & Hood, 2006) CB3.3C (Upper Bay) CB5.3 (Mid-bay) C6.3 (Lower Bay) Chlorophyll Dissolved Oxygen DON, PON Freshwater Flux NO 3 /NO 2 /NH 4 TSS

Aquatic Sciences, 20 February 2013 Chesapeake Bay Ecological Prediction System (CBEPS) 1) Ocean Quality Control System (OQCS) Automatic retrieval of historical and real-time data for validation and model forcing 2) Ocean Hydrodynamic Modeling System (OHMS) ChesROMS and Empirical Habitat Models 3) Ocean Model Assessment System (OMAS) Skill assessment of model predictions against data acquired by OQCS 4) Ocean Model Dissemination System (OMDS) Data archive and forecast dissemination Utilizes data interoperability techniques to facilitate efficient provision of model results to end users Brown, et al., J. Mar. Sys., 2013.

Aquatic Sciences, 20 February 2013 BGC Modeling Targets & Implementation Goals 1) Phytoplankton Bloom Dynamics Capture Spatio-temporal Physical-Biogeochemical Interactions Associated with Estuarine Circulation 2) Particulate and Dissolved Constituents N-cycling Linkage of Water Column & Benthos 3) Dissolved Oxygen Evolution Denitrification Onset - Offers Insight into N Balances & Budget Hindcast Year Chosen for Model Implementation is 1999 (“Typical” Conditions; Model Physics Validated) Xu, et al., Est. and Coasts., Improved ChesROMS BGC Realism -> More Robust Ecological Forecast System (CBEPS)

Aquatic Sciences, 20 February 2013 ChesROMS Biogeochemical Flows 1) Benthic NH 4 Efflux & NO 3 Uptake ramp up as overlying DO decreases 2) Reduce POM sinking in bottom layer i) Promote O 2 Demand in Water Column ii) Promote BGC link to Estuarine Circulation 1) Reduce D L Sinking Velocity 2) Particle Aggregation (Stickiness) i) Regulates Bloom Dynamics, POM Loads & Sinking/Export of Organic Matter ii) Tends to Degrade O 2 Evolution (WC DO Increases) Sensitivity Explorations Aspects of Implementation Overcome “Tension” in BGC Mechanisms Bloom Dynamics Hypoxia Realism DIN Concentrations Bloom Dynamics Overall Goals DO is Indicated by the Light Blue Background

Aquatic Sciences, 20 February 2013 Summary of Sensitivity Studies Test 64 -> 85: ⬇ D L Sink Velocity (0.5 x); ⬆ Max Nitrification Rate (4x) Test 64 -> 91: Constant Phytoplankton Growth Rate Test 91 -> 96: ⬇ Non-Dim Zooplankton Growth Rate (0.8x) Test 96 -> 100: ⬆ Coagulation Param (1.5x) Test 91 -> 104: Zooplankton Grazing ≠ f(Temperature) Test 100 -> 105: ⬇ D L Sink Velocity (0.5 x) 1CB2.2 2CB3.1 3CB3.2 4CB3.3C 5CB4.1C 6CB4.1W 7CB4.2W 8CB4.3C 9CB4.3W 10CB4.4 11CB5.1 12CB5.2 13CB5.3 14CB5.4W 15CB5.5 16CB6.1 17CB6.3 18CB6.4 19CB7.1 20CB7.1N 21CB7.1S 22CB7.2 23CB7.2E 24CB7.3 IndexStation ChlorophyllAmmonium NitrateDO

Aquatic Sciences, 20 February 2013 Hypoxic Volume (km 3 ) Comparisons Initial Baseline Solution (Test 64) Test 64 -> 85: ⬇ D L Sink Velocity (0.5 x); ⬆ Max Nitrification Rate (4x) Test 91 -> 96: ⬇ Non-Dim Zooplankton Growth Rate (0.8x) New Baseline Solution (Test 105) 1) Extension of Hypoxic Volume Envelope for Model Overall, the 4 mg/ml threshold is a closer fit to the CBP-based Hypoxic Volume Seasonal variability consisting of onset and dissipation timing are reasonable

Aquatic Sciences, 20 February 2013 Baseline Solution ChlorophyllDissolved Oxygen Upper Bay (4.1C) Upper Bay Mid-Bay (5.3) Mid-Bay Lower Bay (6.3) Lower Bay

Aquatic Sciences, 20 February 2013 Extending the Model Ideally, Phys-BGC Model Will Naturally Capture Interannual Variability or Model Provides Additional Insights into the Chesapeake System

Aquatic Sciences, 20 February 2013 Summary 1) Retain Organic Matter in Water Column Promotes Water Column Oxygen Demand (to a point) BUT! Oxic N-cycling Promotes O 2 Production 2) Model Suggests a “Pulsing” of low DO conditions in bottom waters through the summer Linkage to variability in modeled phytoplankton biomass Refining Hypoxic Fidelity in the Model 3)How to Amplify Denitrification in the Water Column and Anoxia Establishment? Adjust the Nitrification - Denitrification Transition Bottom Dissolved Oxygen Chesapeake Bay System and Availability of CBP Data Provide an Ideal Proving Ground for Development of the Biogeochemical Module

Aquatic Sciences, 20 February 2013 Thank You!