Advanced microwave sounding unit

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The advanced microwave sounding unit (AMSU) is a multi-channel microwave radiometer installed on meteorological satellites. The instrument examines several bands of microwave radiation from the atmosphere to perform atmospheric sounding of temperature and moisture levels.

Contents

Flooding from Hurricane Isidore shown by AMSU channel 2 Isidore flooding diff.jpg
Flooding from Hurricane Isidore shown by AMSU channel 2

Products

Level-1 radiance data are calibrated brightness temperatures.

Level-2 geophysical data from AMSU include:

AMSU data is also used together with infrared radiances from HIRS, AIRS, or IASI to produce blended MW/IR level-2 geophysical products such as:

Applications

AMSU data is used extensively in weather prediction. Brightness temperatures are processed as quickly as possible and sent to numerical weather prediction (NWP) centers around the world. This data helps keep the assessment of the current state of the atmosphere correct, which in turn helps make predictions more accurate.

Long-term AMSU records are also used in studies of climate.

History

AMSU-A + AMSU-B have flown together on the 3 NOAA KLM satellites: NOAA-15 (NOAA K), launched May 13, 1998; NOAA-16 (NOAA L), launched September 21, 2000; and NOAA-17 (NOAA M), launched June 24, 2002.

For NOAA-18 (NOAA N), launched May 20, 2005, AMSU-B was replaced by a similar instrument, the Microwave Humidity Sounder (MHS).

Versions of AMSU-A also fly on the NASA Aqua Earth science satellite and the EUMETSAT MetOp series. On these spacecraft, AMSU-B is replaced by similar microwave humidity sounders: HSB for Aqua and MHS for MetOp.

The AMSU was an improvement of the Microwave Sounding Unit (MSU), incorporating capabilities of the Stratospheric Sounding Unit (SSU), both of which had flown on TIROS-N in 1978 and continued on the NOAA-6 through NOAA-14 satellites. The next generation in the family is the Advanced Technology Microwave Sounder (ATMS), first flown on Suomi-NPP in 2011 and now standard equipment on the JPSS series of satellites, the first of which, NOAA-20, launched in 2017.

AMSUs were manufactured by Aerojet Corporation in Azusa, California. This organization is now part of Northrop Grumman Electronic Systems.

Observation geometry

AMSUs are always situated on polar-orbiting satellites in Sun-synchronous orbits. This results in their crossing the equator at the same two local solar times every orbit. For example, EOS Aqua crosses the equator in daylight heading north (ascending) at 1:30 pm solar time and in darkness heading south (descending) at 1:30 am solar time.

The AMSU instruments scan continuously in a "whisk broom" mode. During about 6 seconds of each 8-second observation cycle, AMSU-A makes 30 observations at 3.3° steps from −48° to +48°. It then makes observations of a warm calibration target and of cold space before it returns to its original position for the start of the next scan. In these 8 seconds the subsatellite point moves about 45 km, so the next scan will be 45 km further along the track. AMSU-B meanwhile makes 3 scans of 90 observations each, with a spacing of 1.1°.

During any given 24-hour period there are approximately 16 orbits. Almost the entire globe is observed in either daylight or nighttime mode, many in both. Polar regions are observed nearly every 100 minutes.

Instrument characteristics

The AMSU has two sub-instruments, AMSU-A and AMSU-B. AMSU-A has 15 channels between 23.8 and 89  GHz, and is used primarily for measuring atmospheric temperatures (known as "temperature sounding"). It has a ground resolution near nadir of 45 km. AMSU-B, with five channels between 89 and 183.3 GHz, has a spatial resolution near nadir of 15 km and is primarily intended for moisture sounding. Spot size of both sub-instruments becomes larger and more elongated toward the edges of the swath. When the two instruments are used together, there are roughly 9 AMSU-B fields-of-view in a 3x3 array corresponding to each AMSU-A field-of-view. This reflects the higher spatial variability of water vapor compared to temperature. HIRS/3 infrared sounders with the same spatial resolution as AMSU-B are also included on NOAA 15–17 satellites and are used together with AMSU-A and AMSU-B. Together the three instruments form ATOVS, the Advanced TIROS Operational Vertical Sounder.

The Aqua and MetOp AMSU-A instruments are 15-channel microwave sounders designed primarily to obtain temperature profiles in the upper atmosphere (especially the stratosphere) and to provide a cloud-filtering capability for tropospheric temperature observations. The EOS AMSU-A is part of a closely coupled triplet of instruments that include the AIRS and HSB. The MetOp AMSU-A similarly works with HIRS, IASI, and MHS. MHS and HSB are variants on AMSU-B.

Table 1 Radiometric characteristics of the AMSU-A (from 3,5).

Channel NumberFrequency

(GHz)

Polarization

(at nadir)

Number

of Bands

Instrument Sensitivity

NEDT (K)

Primary Function
123.8vertical10.30Water Vapor Burden
231.4vertical10.30Water Vapor Burden
350.3vertical10.40Water Vapor Burden
452.8vertical10.25Water Vapor Burden
553.596 ± 0.115horizontal20.25Tropospheric Temperature
654.4horizontal10.25Tropospheric Temperature
754.94vertical10.25Tropospheric Temperature
855.5horizontal10.25Tropospheric Temperature
957.290horizontal10.25Stratospheric Temperature
1057.290 ± 0.217horizontal20.40Stratospheric Temperature
1157.290 ± 0.3222 ± 0.048horizontal40.40Stratospheric Temperature
1257.290 ± 0.3222 ± 0.022horizontal40.60Stratospheric Temperature
1357.290 ± 0.3222 ± 0.010horizontal40.80Stratospheric Temperature
1457.290 ± 0.3222 ± 0.0045horizontal41.20Stratospheric Temperature
1589.0vertical10.50Cloud Top/Snow

Table 2 Radiometric characteristics of the AMSU-B (from 4).

Channel NumberFrequency

(GHz)

Polarization

(at nadir)

Number

of bands

Instrument Sensitivity

NEDT (K)

1689.9 ± 0.9vertical20.37
17150 ± 0.9vertical20.84
18183.31 ± 1.00vertical21.06
19183.31 ± 3.00vertical20.70
20183.31 ± 7.00vertical20.60

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