Surface Current Mapping with High Frequency RADAR.

Slides:



Advertisements
Similar presentations
Teresa Garner Larry Atkinson. Introduction to HFRADAR Sites & Data Circulation in the Bay Tidal Sub-tidal Quality Control Efforts Instrument Comparisons.
Advertisements

Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Measuring Two-Dimensional Surface Velocity Distribution
L. K. Shay, J. Martinez-Pedraja , A. B. Parks
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Influence of Antenna Pattern Distortions on Surface Current Data collected by a CODAR HF-Radar System Josh T. Kohut Scott M. Glenn Donald E. Barrick.
IOOS, NOAA and HF Radar QA/QC and Standards Jack Harlan National Ocean Service Center for Operational Oceanographic Products and Services QARTOD
Modeling Larval Connectivity for the SoCal Bight Satoshi Mitarai, James Watson & David Siegel Institute for Computational Earth System Science University.
Surface Current Mapping in the Lower Chesapeake Bay Larry Atkinson Teresa Garner Jose Blanco.
QARTOD 2: Remote Currents Working Group Definitions: Level 1 – refers to radials Level 2 – refers to total vectors Level 3 – refers to higher level data.
Remote Sensing: John Wilkin Active microwave systems (4) Coastal HF Radar IMCS Building Room 214C ext 251 Dunes of sand.
Remote Sensing: John Wilkin Active microwave systems Coastal HF Radar IMCS Building Room 214C ph: Dunes of sand and seaweed,
SeaSonde Overview.
Upstream Engineering Centre Ocean predictions and the oil and gas industry - room for improvement? Colin Grant Metocean Technical Authority.
Assessment and Quantification of HF Radar Uncertainty Fearghal O’Donncha Sean McKenna Emanuele Ragnoli Teresa UpdykeHugh Roarty.
Indian Ocean Forecast System (INDOFOS) Francis P. A. Earth System Sciences Organisation (ESSO) Indian National Centre for Ocean Information Services (INCOIS)
Abbie Harris - NOAA Ocean Acidification Think Tank #5 Current and Future Research at the Institute for Marine Remote Sensing Abbie Rae Harris Institute.
The Gulf of Maine Ocean Observing System. Technical Program Real time monitoring and forecasts of: Weather - surface ocean winds, air temperature, visibility.
Cape Cod Cape Hatteras NJ MA CT VA DE NY NC RI MD PA M ID - A TLANTIC R EGIONAL A SSOCIATION C OASTAL O CEAN O BSERVING S YSTEM 1000 km Cape to Cape RAISING.
National High Frequency Radar Network Jack Harlan, Ph. D. NOAA IOOS Program Office Project Manager: HF Radar DHS Training 21 Apr 2010 Washington, DC.
Surface Currents off the Outer Banks of North Carolina Luke Stearns, UNC Chapel Hill.
Ligurian Sea Mid-Atlantic Bight Results from the Mid Atlantic High Frequency Radar Network Radar Network Hugh Roarty, Scott Glenn, Josh Kohut, Erick Rivera,
SCM 330 Ocean Discovery through Technology Area F GE.
CODAR Ben Kravitz September 29, Outline What is CODAR? Doppler shift Bragg scatter How CODAR works What CODAR can tell us.
Interdisciplinary Integration and Research Directions CMOP possesses a wide range of interdisciplinary research assets - Biological - Chemical - Physical.
Surface Current Mapping in the Lower Chesapeake Bay.
0 0 Figure 3. Near real-time comparisons of 6 minute NOAA ADCP data (blue) and hourly CODAR data (red) at (YS) York Spit (CH) Cape Henry and (TS) Thimble.
Using A Fleet of Slocum Battery Gliders in a Regional Scale Coastal Ocean Observatory Elizabeth L. Creed, Chhaya Mudgal, Scott M. Glenn and Oscar M. Schofield.
L. K. Shay 1, J. Martinez-Pedraja 1, B. K. Haus 1, Brad Parks 1, Peter Vertes 1, Lew Gramer 2, and J. Brewster 1 1 Division of Meteorology and Physical.
CONRAD BLUCHER INSTITUTE ACTIVITIES SUPPORTING TEXAS PORTS AND WATERWAYS OPERATIONS Two Inter-related Services to the Port Community: 1. The Texas Coastal.
SCCOOS Goals and Efforts Within COCMP, SCCOOS aims to develop products and procedures—based on observational data—that effectively evaluate and improve.
Surface Current Mapping in the Lower Chesapeake Bay INTRODUCTION High frequency RADAR antennas are used to observe the surface circulation patterns in.
Ocean Wave and Current Radars By Laura Elston. Our earth is a very aqueous environment with nearly three quarters of it covered by ocean. So how do we.
AWIPS-2 HF Radar Sea-Surface Current Product By Ross Van Til Contributions by: Nicole Kurkowski, OS&T Dr. Pablo Santos, WFO Miami Dr. Jack Harlan, NOAA.
Sang-Ho Lee*, Hong-Bae Moon, Chang-Soo Kim Dept. Oceanography, BK21 Team, Kunsan Nat’l Univ., Korea Accuracy of currents measured by HF radar in the coastal.
The VIEW antenna is located on an open beach and is more isolated from structures which can cause distortion; therefore, its pattern shape is similar to.
CALYPSO Project FINAL MEETING PROJECT SEMINAR University of Malta, Valletta Campus, Old University Building, St Paul Street, Valletta 29 August 2013 Beyond.
Application of Radial and Elliptical Surface Current Measurements to Better Resolve Coastal Features  Robert K. Forney, Hugh Roarty, Scott Glenn 
Ensemble-based Assimilation of HF-Radar Surface Currents in a West Florida Shelf ROMS Nested into HYCOM and filtering of spurious surface gravity waves.
Great Lakes Environmental Research Laboratory Review – Ann Arbor, MI November 15-18, Click to edit Master text styles –Second level Third level.
Hindcast Simulations of Hydrodynamics in the Northern Gulf of Mexico Using the FVCOM Model Zizang Yang 1, Eugene Wei 1, Aijun Zhang 2, Richard Patchen.
REAL-TIME ESTIMATION OF OCEAN WAVE FIELDS FROM MARINE RADAR DATA David R. Lyzenga, Okey G. Nwogu, and Robert F. Beck University of Michigan, Ann Arbor,
1 Storms activity: wave modelling and atmospheric circulation Part 1. Wave modelling. V. Arkhipkin 1, S. Myslenkov 1 Part 2. Atmospheric circulation. A.
Ocean Surface Current Observations in PWS Carter Ohlmann Institute for Computational Earth System Science, University of California, Santa Barbara, CA.
Figure 2. Near real-time comparisons of 6 minute NOAA ADCP data (blue) and hourly CODAR data (red) at (YS) York Spit (CH) Cape Henry and (TS) Thimble Shoals.
The California Current System from a Lagrangian Perspective Carter Ohlmann Institute for Computational Earth System Science, University of California,
NOAA and HF Radar FY05 and Beyond Jack Harlan National Ocean Service Center for Operational Oceanographic Products and Services SCCOOS Meeting 18 October.
Surface Current Mapping in the Lower Chesapeake Bay INTRODUCTION High frequency RADAR antennas are used to observe the surface circulation patterns in.
1 Modeling and Forecasting for SCCOOS (Southern California Coastal Ocean Observing System) Yi Chao 1, 2 & Jim McWilliams 2 1 Jet Propulsion Laboratory,
CASE #3: Floating Away The Situation: While entering New York Harbor, several boxes of rubber ducks fell off their cargo ship. Using the data provided,
Real-Time Beyond the Horizon Vessel Detection
QA/QC Methods for 13 MHz Brant Beach (BRNT) Test Case
Validation of an ultra high frequency radar (River sonde) for current mapping in the urbanized Hudson River estuary 2010 summer research institute at.
Results from the Mid Atlantic High Frequency Radar Network
Evaluation of Three Antenna Pattern Measurements for a 25 MHz SeaSonde
Surface Current Mapping in the Lower Chesapeake Bay
A Closer Look at CODAR HF Radar Spectra
Bistatic Systems: Preparing for Multistatic
Mapping Technology.
Application of 13 MHz SeaSonde Systems for Vessel Detection
Hugh Roarty, Michael Smith, Ethan Handel and Scott Glenn
Robert K. Forney, Hugh Roarty, Scott Glenn March 5th, 2015
Quality Assurance Measures for High Frequency Radar Systems
Analysis of the Wind Resource off New Jersey for Offshore Wind Energy Development Hugh Roarty, Joe Riscica, Laura Palamara, Louis Bowers, Greg Seroka,
HF Radar Systems Engineering Plan
October 27, 2011 New Brunswick, NJ
LCDR George Wright, USN OC 3570 – Winter 2008 Friday, March 14th 2008
A Multi-static HF Radar Network for the
Observing the Ocean from the Rutgers University “COOL Room”
Coastal Ocean Dynamics Radar (CODAR) Mapping of
Presentation transcript:

Surface Current Mapping with High Frequency RADAR

Applications Search and rescue Navigation Pollution Tracking (Oil spills, red tides, …) Recreational boating Fishing Assimilation into numerical circulation models to improve nowcast/forecast capabilities

Study Area & Antenna Sites Source: U.S. Geological Survey ( Source:

Chesapeake Bay Bridge Tunnel (CBBT) Ocean View Community Beach (VIEW) AT OUR FIELD SITES 25.4 MHz CODAR Standard Range Antennas with co-located Tx/Rx MiniMac Field Computers Cell phone/Cable modem connections

Operating Costs Equipment (antenna, computer, electronics enclosure, software) roughly 150K / site Power / network connections / access to the site –CBBT $220/ month –VIEW $100/ month Technician Additional costs: Pattern measurements

Data Products Updated Hourly Sub-tidal Flow Trajectories ( Time Series Hourly Velocity

Shipping Channels

HF RADAR National Network UCSD, Scripps Institute

½ λ f = 25MHz λ=12m Water speed is determined using the frequency shift, f s, in the return signal. f obs =25 + f s f=25 Ocean waves with strongest return signal Antenna

Radial Current Velocities… are combined on a grid Mapping requires at least two antennas! A single antenna measures only one component of the water velocity, the speed of the water moving directly towards or away from it. Radial vectors are output in range bins of 1.5 km and directional bins of 5 degrees. The grid is designed by the operator.

Grid for Total Current Vectors 2 km Grid courtesy of CORDC National Network Preserves orthogonality Red points fail stability angle requirements Baseline

Gridpoint 2.5 km Radial Current Velocities Total Current Velocities Around each grid point… Combine Radial Vectors (Least Squares Average) + Grid

Data Quality Calibration and Radial Coverage

Antenna PatternsRadial Coverage CBBT VIEW

Challenges At a 360° site, antenna pattern measurement is essential Antenna isolation Summertime heat Interference (Natural & Man-made)

Baseline (consistency) Tide Moored ADCP Towed ADCP Data Validation by Comparison Photo Source: NOAA OSTEP report

Baseline Comparisons Ideal antenna patternsMeasured antenna patterns

Tidal Analysis

Moored ADCP Comparison (CH) (TS) (YS) SiteMeanS.Dev Cape Henry Thimble Shoals York Spit Red line = CODAR Blue line = NOAA ADCP Black = |NOAA-CODAR| Difference Statistics

Bistatic system: enhance coverage by using precise timing so that Rx can receive sea scatter from another transmitter (e.g. on a buoy) RiverSonde Ship detection Shallow water waves CODAR Current Research & Development Source: CODAR Research & Development poster

Our Future Plans Incorporate data into GIS; map with other regional spatial data Continue to work with trajectories/ plume tracking Model comparisons Outreach (VA Aquarium, education) Web page & product development –Shipping channels –Ocean View beaches ChesROMS model output AVHRR SST Daily Composite, September 24, 2007 from NOAA Coastwatch

Acknowledgements Larry Atkinson and Jose Blanco CIT, MACOORA, NOAA CODAR support Advice and assistance from numerous other HF RADAR operators