X-Band Lightweight Rainfall Radiometer (LRR-X)

Aircraft Sensor Specifications
Strategic Advantages
CLICK ON A LINK BELOW TO SEE PHOTOS OF LRR BEING BUILT
LRR System Calibration
On board calibration provides ~2K absolute TB and ~0.2K stability
Inject correlated noise between each antenna and receiver for grains
Switch each channel to uncorrelated reference loads for offset
Anechoic Chamber measurement of interference patterns
Determines relative spatial frequency response to each antenna pair
Clear sky ocean radiobrightness model for end-to-end absolute calibration
Determines system gain (noise diode TBinjected) and offset (antenna ohmic losses) calibration parameter
Demonstrated operationally with TOPEX and Jason-1 Microwave Radiometers
~1.0K accuracy and ~0.3K long term stability
Interferometric Aperture Synthesis
Cross-correlation of signals from pairs of antennas with
different baselines samples visibility
function
Visibility function is Fourier transform of brightness temperature distribution of scene
Used in radio astronomy since 1950s
First used in Earth Remote Sensing by ESTAR to measure sea surface salinity & soil moisture
ESA SMOS Mission (launch ~2007) will be first spaceborne mission that will use technique
Successful first aircraft flight demo of LRR-X in June 2003
LRR First Field Campaign -- Summary
Integration onto DC-8, 12-17 May 2003
other sensors: JPL PR-2 (precip radar), JPL WindRad & PolScat (ocean surface wind vector), LaRC et al. DICE (in situ aerosols, aerosol lidar)
Shakedown Flights, 28-29 May 2003
air dam added in front of LRR to reduce turbulence
Engineering Check Flights, 29 May & 3 June 2003
ground beacon overflights confirm image impulses response
WindSat Cal/Val Flights, 5 & 11 June 2003
Navy Coriolis cal/val overpasses
Precipitation and Mapping science Flights, 12 & 13 June 2003
Coastal Imaging, WA Cascade Range snowfall, Pac NW precip
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