AMPR
Point of Contact:
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Robbie Hood
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Global Hydrology and Climate Center
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NASA/ Marshall Space Flight Center/ Code: SD60
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Huntsville, Alabama 35805
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Office Telephone: (256) 961-7956
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FAX: (256) 961-7723
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E-mail: robbie.hood@msfc.nasa.gov
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AMPR Home Page: http://wwwghcc.msfc.nasa.gov/ampr/
Brief Instrument Description of the
Advanced Microwave Precipitation Radiometer (AMPR)
INTRODUCTION
The Advanced Microwave Precipitation Radiometer (AMPR) remotely senses
passive microwave signatures of geophysical parameters from an airborne
platform. The instrument is a low noise system which can provide multifrequency
microwave imagery with high spatial and temporal resolution. AMPR data
are collected at a combination of frequencies (10.7, 19.35, 37.1, and 85.5
GHz) unique to current NASA aircraft instrumentation. These frequencies
are well suited to the study of rain cloud systems, but are also useful
to studies of various ocean and land surface processes. Additionally, the
aircraft information collected at these frequencies offer a rich data base
for satellite simulations of the current Defense Meteorological Satellite
Program (DMSP) Special Sensor Microwave/Imager (SSM/I), the NASA Tropical
Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) scheduled for
launch in 1997, and the Advanced Microwave Scanning Radiometer (AMSR) planned
to fly aboard the Earth Observing System (EOS) PM-1 platform.
INSTRUMENT DESCRIPTION
The AMPR is a total power scanning multifrequency passive radiometer
which collects data at 10.7, 19.35, 37.1, and 85.5 GHz. The AMPR is currently
configured to fly aboard a NASA ER-2 aircraft which has an approximate
cruising altitude of 20 km. The radiometer and accompanying data system
are mounted behind the cockpit in the Q-bay section of the fuselage. The
radiometer is positioned in the lower Q-bay with the scanning mirror extending
below the body of the aircraft into a hatch with a porthole open to the
ambient atmosphere. The data system is mounted above the radiometer in
the upper Q-bay section.
The AMPR is composed of two adjacent antenna systems with one large
scanning mirror accommodating both systems. One antenna system was designed
to use a copy of the SSM/I feedhorn for the three higher frequencies. The
second antenna system collects data at 10.7 GHz using a feedhorn designed
by Georgia Tech Research Institute (GTRI).
The ground spatial resolution of the nadir footprint from the nominal
aircraft altitude of 20 km is 0.6 km for the 85.5 GHz channel, 1.5 km for
37.1 GHz, and 2.8 km for both the 19.35 and 10.7 channels The AMPR calibrates
with external cold and warm loads after every fourth data scan. A total
calibration sequence or a total data scan are each performed in a three
second time period. The AMPR scanner sweeps through a total 90o (+/- 45o
from nadir) data scan collecting a sample for each channel every 1.8o for
a total of 50 samples per channel. Based upon an aircraft altitude of 20
km and an aircraft speed of 200 ms-1, this scan rate will yield contiguous
footprints for the 85.5 GHz channel within a 40 km wide swath. The other
three channels will be oversampled by the factors given in Table 1 which
also lists other performance characteristics of the radiometer. The alignment
of the feedhorns has been adjusted such that vertical polarization is received
45o to the left of nadir and horizontal is received 45o to the right of
nadir. An equal mixture of vertical and horizontal polarizations is received
at nadir.
|
Frequency
|
IF
Bandwidth
|
3 dB
Beamwidth
|
Oversampling
|
Mainbeam
Efficiency
|
Cross-
Polarization
|
|
85.5 GHz
|
1400 MHz
|
1.8o
|
1.0x
|
93.2%
|
1.4%
|
|
37.1 GHz
|
900MHz
|
4.2o
|
2.3x
|
98.8%
|
0.4%
|
|
19.35 GHz
|
240 MHz
|
8.0o
|
4.4x
|
98.7%
|
1.6%
|
|
10.7 GHz
|
100MHz
|
8.0o
|
4.4x
|
97.8%
|
0.2%
|
Table 1. AMPR instrument characteristics
|