Results of First Flight Tests of the WSRA Wide Swath Radar Altimeter Ivan PopStefanija [email protected]ProSensing Inc. 107 Sunderland Rd. Amherst, MA 01002 USA, 63 rd Interdepartmental Hurricane Conference Peter Black NRL/SAIC Inc. 7 Grace Hopper Ave. Monterey, CA 93943 Edward J. Walsh NASA Goddard Space Flight Center, Greenbelt, MD 20771
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Results of First Flight Tests of the WSRA W ide S wath R adar A ltimeter
63 rd Interdepartmental Hurricane Conference. Results of First Flight Tests of the WSRA W ide S wath R adar A ltimeter. Ivan PopStefanija [email protected] ProSensing Inc. 107 Sunderland Rd. Amherst, MA 01002 USA,. Peter Black NRL/SAIC Inc. 7 Grace Hopper Ave. - PowerPoint PPT Presentation
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Results of First Flight Tests of the WSRA
Wide Swath Radar Altimeter
Ivan PopStefanija [email protected] ProSensing Inc. 107 Sunderland Rd. Amherst, MA 01002 USA,
63rd Interdepartmental Hurricane Conference
Peter BlackNRL/SAIC Inc.7 Grace Hopper Ave.Monterey, CA 93943
Edward J. WalshNASA Goddard Space Flight Center, Greenbelt, MD 20771
April 29, 2008 28th Conference on Hurricanes and Tropical Meteorology 2
Operational SRA Why?
Mapping ocean wave height (surface topography) within the inner core of hurricanes
Measurement of directional ocean wave spectra
Real-time reporting of 12-foot seas radius
Improved forecasting of hurricane development
NASA’s SRA prototype has demonstrated instrument feasibility NASA’s SRA prototype has demonstrated instrument feasibility and data product utility and data product utility operational SRA on multiple aircraft operational SRA on multiple aircraft will provide routine data to enhance hurricane forecastingwill provide routine data to enhance hurricane forecasting
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Who can benefit?
NOAA Tropical Prediction Center / National Hurricane Center
Fulfilling operational requirements for wave height and extent of 12 foot sea height radius
National Centers for Environmental Prediction
Development of comprehensive Hurricane Weather Research and Forecasting (HWRF) model SRA data used for modeling of the wave field and surface roughness
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Baseline Technology
Prototype Scanning Radar Altimeter (SRA) was funded through NASA’s Advanced Application Flight Experiment (AAFE) program since 1973
SRA prototype has flown on NOAA’s WP-3D aircraft in every hurricane season since 1998 [retired 2005]
NASA has developed a comprehensive SRA processing software: Transforms wave topography data into
directional ocean wave spectra Extracts pertinent wave information Transmits wave information to the NHC
Sequential transmission and collection of raw I&Q data for each of 62 antenna array elements.
Performing de-chirping FFT on each of the 62 I&Q vectors. Averaging coherently subsequent frames of 62 vectors with the coherent
integration time equivalent of the antenna traveling a distance of about 60 cm.
Multiplying the data with correction coefficients. Performing the digital beam forming FFT at each range gate. Calculating the magnitude (power) for the each beam return. Figure 15 shows
the radar return for one beam at nadir. This creates a “frame”. Averaging frames together to reduce signal fading. The averaging was set to
generate 10 averaged frames per second.
April 29, 2008 28th Conference on Hurricanes and Tropical Meteorology 9
WSRA Data Quality
WSRA has expanded the operational range of the measurement conditions over the retired NASA prototype SRA
WSRA has obtained usable signal from a significantly higher altitudes (12,500 feet vs 5,000 feet).
WSRA signal was not significantly attenuated even under high rain rate conditions often found in hurricanes.
WSRA has demonstrated its capability to measure ocean wave spectra under a variety of wind conditions.