The AMPR is a total power passive microwave radiometer producing calibrated brightness temperatures (TB) at 10.7, 19.35, 37.1, and 85.5 GHz. These frequencies are sensitive to the emission and scattering of precipitation-size ice, liquid water, and water vapor. The AMPR performs a 90º cross-track data scan perpendicular to the direction of aircraft motion. It processes a linear polarization feed with full vertical polarization at -45º and full horizontal polarization at +45º, with the polarization across the scan mixed as a function of sin2, giving an equal V-H mixture at 0º (aircraft nadir). A full calibration is made every fifth scan using hot and cold blackbodies. From a typical ER-2 flight altitude of ~20 km, surface footprint sizes range from 640 m (85.5 GHz) to 2.8 km (10.7 GHz). All four channels share a common measurement grid with collocated footprint centers, resulting in over-sampling of the low frequency channels with respect to 85.5 GHz.
Advanced Microwave Precipitation Radiometer
Instrument Type
Measurements
Aircraft
Recent Missions
Point(s) of Contact
Range of Measurement
Ground
Instrument Pointing
Cross-track scanning
Measurement Wavelengths
10.7 GHz,
19.35 GHz,
37.1 GHz,
85.5 GHz
Notes
AMPR measures passive microwave radiation from 10 to 85 GHz
Website
Data Website
Publications
Hood, R., et al. (2006), Classification of Tropical Oceanic Precipitation using High-Altitude Aircraft Microwave and Electric Field Measurements, J. Atmos. Sci., 63, 218-233.
McFarquhar, G.M., et al. (2006), Factors Affecting the Evolution of Hurricane Erin (2001) and the Distributions of Hydrometeors: Role of Microphysical Processes, J. Atmos. Sci., 63, 127-150.
Jackson, G.S., et al. (2003), Combined Radiometer/Radar Microphysical Profile Estimations with Emphasis on High-Frequency Brightness Temperature Observations, J. Appl. Meteor., 42, 476-487.
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