Mr. Robert Forney Dr. Hugh Roarty Dr. Scott Glenn Measuring Waves with a Compact HF Radar MTS/IEEE OCEANS15 October 2015 Washington DC.

Slides:



Advertisements
Similar presentations
Think & Solve Problems Chapter 26
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
Homework.
Wavelength The distance between one point on a wave and another point exactly like it.
Crest- highest part of a wave Trough- lowest part of a wave Wavelength- horizontal length between crests. Wave height- vertical distance from crest to.
Specular reflectorquasi-specular reflector quasi-Lambert reflector Lambert reflector Limiting Forms of Reflection and Scatter from a Surface.
Ocean Connections: Mapping potential pathways between the spill in the Gulf of Mexico and the Jersey Shore Dr. Josh Kohut Rutgers University School of.
Wave Measurements from SeaSondes. Measurements Significant Wave Height Wave Period Peak Wave Direction Wind Direction.
Success Stories – Making a Difference Optimizing HF Radar for SAR using USCG Surface Drifters Art Allen U.S. Coast Guard Josh Kohut, Scott Glenn Rutgers.
Types Ocean Observations and Weather Information Wave Height and Frequency Current Weather Synoptic Situation Atmospherics (Temp, Winds, Barometric Pressure,
Cape Cod to Cape Hatteras: ~1000 km Coastline Results from the Mid Atlantic High Frequency Radar Network Hugh Roarty, Ethan Handel, Erick Rivera, Josh.
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,
Long-Term Ambient Noise Statistics in the Gulf of Mexico Mark A. Snyder & Peter A. Orlin Naval Oceanographic Office Stennis Space Center, MS Anthony I.
SeaSonde Overview.
National Oceanic and Atmospheric Administration
Assessment and Quantification of HF Radar Uncertainty Fearghal O’Donncha Sean McKenna Emanuele Ragnoli Teresa UpdykeHugh Roarty.
CALYPSO Seminar, 29 th of August of 2013 “Recent advances in the application of SeaSonde HF Radar technology to improve Operational Oceanography capacity”
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.
Surface Current Mapping with High Frequency RADAR.
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.
Waves n Characteristics of All Wind-generated Waves n Deep Water Waves n Shallow Water Waves n Other Water Waves.
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.
What is the wavelength? What is the amplitude?.
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.
Application of Radial and Elliptical Surface Current Measurements to Better Resolve Coastal Features  Robert K. Forney, Hugh Roarty, Scott Glenn 
Floating Offshore Wind Turbines Floating Offshore Wind Turbines An Aeromechanic Study on the Performance, Loading, and the Near Wake Characteristics of.
1. A wave passes every seconds. What is the frequency with which waves pass? (80.0 Hz)
Look at your formula chart for question 9 10.
Ocean Surface Current Observations in PWS Carter Ohlmann Institute for Computational Earth System Science, University of California, Santa Barbara, CA.
L. K. (Nick) Shay, J. Martinez-Pedraja and M. Archer Department of Ocean Sciences, RSMAS To improve our understanding of surface processes and their linkages.
Physical Conditions 9/16-9/ including Hurricane Isabel inches Hg ft (MLLW) knots inches Atmospheric Pressure.
Ocean Currents. Mass movement or flow of ocean water Mass movement or flow of ocean water River within the ocean River within the ocean Two types Two.
V f λ.
1 Experimental Study of the Microwave Radar Doppler Spectrum Backscattered from the Sea Surface at Small Incidence Angles Titchenko Yu. A., Karaev V. Yu.,
Surface Current Mapping in the Lower Chesapeake Bay INTRODUCTION High frequency RADAR antennas are used to observe the surface circulation patterns in.
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
MARACOOS High Frequency Radar Network Operations
Bistatic Systems: Preparing for Multistatic
Speed Formula - Waves.
Application of 13 MHz SeaSonde Systems for Vessel Detection
OCG High Frequency Radar
Hugh Roarty, Michael Smith, Ethan Handel and Scott Glenn
V f λ.
Robert K. Forney, Hugh Roarty, Scott Glenn March 5th, 2015
Chapter 20.
Colin Evans, Hugh Roarty, Scott Glenn, Josh Kohut
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,
Recognizing First and Second Order Features
Essential Question: What are the types and properties of waves?
October 27, 2011 New Brunswick, NJ
Calculating Wave Speed
What we will do today: Carry out calculations involving the relationship between speed, wavelength and frequency for waves.
OC3570 Project Winter 2007 A COMPARISON OF COASTAL CURRENTS USING LAND BASED HF RADAR AND SHIP BOARD ADCP OBSERVATIONS LCDR Steve Wall, RAN.
LCDR George Wright, USN OC 3570 – Winter 2008 Friday, March 14th 2008
An Ocean Current Monitoring System for Coastal New Jersey
A Multi-static HF Radar Network for the
by ENS William C. Blodgett, Jr. 22MAR02
Coastal Ocean Dynamics Radar (CODAR) Mapping of
COMPARISON OF COASTAL CURRENTS FROM HF RADAR AND ADCP DATA
Southern California Coastal Ocean Observing System (SCCOOS) HF RADAR Network “SCCOOS brings together coastal observations in the Southern California Bight.
Presentation transcript:

Mr. Robert Forney Dr. Hugh Roarty Dr. Scott Glenn Measuring Waves with a Compact HF Radar MTS/IEEE OCEANS15 October 2015 Washington DC

MARACOOS HF RADAR NETWORK 5 MHz13 MHz25 MHz U Mass WHOI U Conn URI Stevens Rutgers Delaware ODU/CIT UNC Stations in Total

Radial Velocity Measurement

Combine Radial Velocity Measurements

Total Vector Surface Current Measurements

Spectra From the Radar

National Waves Plan LocationNew Sensors Total Acquisition Cost Unit Acquisition Cost Offshore13$3.9M$300,000 Outer Shelf17$3.9M$229,000 Inner Shelf19$2.3M$120,000 Coastal66$7.9M$120,000

West Coast HF Radar Measurements Average correlation with wave buoys: 0.88 Root mean square difference: 0.53 m Standard Deviation of difference:0.48 m 2011 Journal of Sensors

West Coast Bathymetry 30 meter isobath Long (2011) used five 13 MHz HF Radars along California coast

Second Order - Waves First Order - Currents

New Jersey Study Area 13 MHz 30 meter isobath BRAD

Range Cell 2 for all HF radar measurements

Bragg Period at 13.5 MHz is XX

Temporal Coverage Feb-Jun 2015 Averaging Time (minutes) Temporal Coverage 3032% 6040% 10043% 12045% 18049%

Frequency (MHz) Sweep Rate (Hz) Doppler Bins Time FFTCSS Avg/Out Radial Avg/Out CSS per Radial File m 04s60/30180/ m 16s15/1075/ m 16s15/1075/307 SeaSonde AcquisitionCSProAnalyze Spectra Existing SeaSonde Settings 15

Radio Frequency (MHz) Radio Wavelength (m) Bragg Wavelength (m) Ocean Wave Period (s) Deep Water Depth (m) Wave Height Saturation (m) Radio Frequency (MHz) Radio Wavelength (ft) Bragg Wavelength (ft) Ocean Wave Period (s) Deep Water Depth (ft) Wave Height Saturation (ft)

October 4, 2015 Nor’easter Hurricane Joaquin

SILD 25 MHz

Wave Height Wave Period

Wave Height Wave Period

SILD 25 MHz Current Wind

RESULTS HF Radars are operating throughout Mid Atlantic and other regions of the US Main focus is for measuring surface currents Secondary application can be for measuring near shore waves