NASA Icing Remote Sensing Andy Reehorst NASA Glenn Research Center Dave Serke NCAR.

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NASA Icing Remote Sensing Andy Reehorst NASA Glenn Research Center Dave Serke NCAR

Transcript of NASA Icing Remote Sensing Andy Reehorst NASA Glenn Research Center Dave Serke NCAR.

NASA Icing Remote Sensing

Andy ReehorstNASA Glenn Research Center

Dave SerkeNCAR

Icing Remote Sensing Goals/Vision

Develop technologies that will enable terminal area sensing and airborne sensing. Implement through incremental development starting at ground-based vertical staring.

Current Capability

Ground-based goal

Airborne goal

Current Focus

Current vertical-pointing Icing R-SNASA Icing Remote Sensing System (NIRSS) Sensors

RadarProvides cloud boundaries

Multi-frequency Microwave RadiometerProvides Temperature ProfileProvides Integrated Water Content

CeilometerRefines cloud base boundary

Current vertical-pointing Icing R-S

Simplified Algorithm

Radar provides cloud profileRadiometer provides temperature profileRadiometer provides integrated liquid water pathDistribute liquid water over cloud extent for LWCDerive droplet size

Reflectivity is a function of both cloud droplet size and liquid water content

Can do this because our water content and radar reflectivity are independent measurements

Use temperature, water content, droplet size to determine icing hazard

Current vertical-pointing Icing R-S

NIRSS (left) and CIP (right) Probability of Detection (POD) (positive and negative) compared to PIREPS.

Altitude/Time plots of NIRSS (top), PiReps (top, red numbers), and CIP (bottom) **Note the larger warning band for CIP**

• Recent comparison of NIRSS and CIP relative to PIREPS• Based upon 3 years of NIRSS data (operating at GRC)

“NIRSS detected almost 80% of positive PIREPs and over 70% of negative PIREPs in a relatively smaller warning volume. CIP detected slightly more positive PIREPs than NIRSS but did fairly poor in detecting negative PIREPs.” From: Johnston, C.J., et al, “Comparison of In-Situ, Model and Ground-Based Inflight Icing Severity”, NASA /TM-2011-217141, Dec 2011.

Current scanning Icing R-S

Sensor Systems

•Radiometrics MP3000A 35 channel Temperature, Water Vapor and Liquid Profiler• 21 channels in K-band 22-30 GHz• 14 channels in V-band 51-59 GHz• Optional Azimuth Positioner• Optional Infrared Thermometer• Located on NASA GRC Icing Research Tunnel balance chamber roof• Vertical and 15 deg slant elevation measurements• Slant measurements made at CLE runway headings• Provides temp profiles and integrated liquid water measurements for vertical

and 15 degree elevations with Radiometrics neural nets

•Radiometrics Narrowbeam Radiometer• Uses Radiometrics’ PR-series receivers• K-band multichannel receiver (21 channels in 22-30GHz)• W-band polarized receiver (89 GHz)• Located on NASA GRC Icing Research Tunnel shop roof• Provides integrated liquid water measurements over all slant angles with

algorithms from Dr. Ulrich Lohnert from the University of Cologne

Current scanning Icing R-S

FEATURES• 1 deg beam widths • Upgraded elevation and azimuth scanning (Moog

Quickset QPT-500)• Integrated Garmin 17 HVS GPS (time) and Vaisala

WXT520 Met (temp, RH, wind, precip)• Rain Mitigation (radiometer lens blower and reflector

hydrophobic coating)

CURRENT PLANS• Install version 3 RadScan software• Install support mod kits

• Changes intended to address operational problems (structure flex, positioner freezes, software bugs)

• Will add tip calibration capability

NASA Narrow-beam Multi-frequency Microwave Radiometer

Developed by Radiometrics, Inc. of Boulder, CO under SBIR and Aviation Safety Program funding