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Stepped Frequency Microwave Radiometer (SFMR)
development
Principal Investigator:
Eric Uhlhorn
Collaborating scientist(s):
Peter Black
Alan Goldstein (AOC)
Ivan Popstefanija (ProSensing Inc.)
Jim Carswell (Remote Sensing Solutions Inc.)
Jimmy Franklin (NHC)
Reports and presentations:
Objective:
Measurement of the hurricane surface wind field, and in particular the
estimation of wind maxima, has long been a requirement of the Tropical
Prediction Center/OAR (TPC/NHC). The
NOAA/Hurricane Research Division's (HRD) Stepped-Frequency Microwave
Radiometer (SFMR)
,built by Prosensing Inc., is the prototype for a new generation
of airborne remote sensing instruments designed for operational
surface wind
estimation in hurricanes. The first experimental SFMR surface wind
measurements were made in Hurricane Allen in 1980,
the first real-time retrieval of winds on board the aircraft in
Hurricane Earl in 1985, and the first operational transmission of
winds to TPC/NHC in Hurricane Dennis in 1999.
Background:
Since hurricane reconnaissance began in 1947, numerous methods have
been employed to estimate the distribution of surface winds in
hurricanes. Sea-state catalogs have provided
a subjective guide for the determination of the wind speed. For many
years surface winds have been estimated by flight-level measurements
using various extrapolation algorithms. Maximum sustained winds have
also been estimated using pressure-wind relationships. Studies prior
to 1980 have shown that passive microwave emissions
from the sea surface are also strongly correlated with wind speed.
The concept for the first experimental SFMR was proposed by C. T.
Swift at the University of Massachusetts Microwave Remote Sensing
Laboratory (UMASS/MIRSL) and built by NASA's Langley Research Center
in 1978. The SFMR design involved a single nadir-viewing antenna and
receiver capable of making measurements of radio emission from the sea
surface at four selectable frequencies between 4.5 and 7.2 GHz. The
"stepping" procedure allowed for estimating the surface wind speed in
hurricanes by correcting for
rain-induced effects in the measurements, and therefore enabling
recovery of the rainrate. The first measurements by the original SFMR
were made from the NOAA WC-130 aircraft in Hurricane
Allen in 1980. By making assumptions about the vertical structure
of the atmosphere together with sea surface temperature (SST)
measurements by a downward-looking airborne infrared radiometer,
reasonable estimates of the ocean surface brightness
temperature (Tb) were made at 4.5, 5.0, 5.6, and 6.6 GHz. Wind
speeds were then calculated assuming a linear increase in wind speed
with Tb, independent of frequency. Agreement between surface (20 m)
winds extrapolated from the 1500 m flight-level and the SFMR
estimates for independent flight legs were within +/-10 %. Despite
the success in Allen, this instrument was never again flown into a
hurricane.
A second SFMR was designed and built in 1982 under the supervision of
C. T. Swift. The number of frequencies was expanded to
six between 4.6 and 7.2 GHz, and the instrument integration time was
reduced to less than one second resulting in improved spatial
resolution. A new retrieval algorithm was also implemented. This instrument was flown on board the
NOAA WP-3D in 1984, and during 12 flights during the 1985 hurricane
season. The SFMR was further modified in 1986 and initially used for
studies of sea-ice structure. Using data obtained
in Hurricanes Earl (1985), Gilbert (1988), and Hugo (1989), the
empirical emissivity/wind speed relationships were refined to include
winds over 60 m/s.
With support from the Office of the Federal Coordinator for
Meteorology (OFCM) the existing horn antenna was replaced with a
dipole array antenna in 1993. The new antenna with a new set of six
frequencies was flown in Hurricane Olivia (1994) and retrieved
high-quality wind estimates. Further funds were provided by OFCM for
an upgrade of the SFMR's receiver, which allowed for increased
calibration stability. The reconfigured SFMR was
first flown in Hurricane Jerry in 1995. Minor modifications were made
to reduce background noise levels after the 1995 season, and since
then the SFMR has flown under this configuration. Following component
failures in 2000, the NOAA Office of Oceanic and Atmospheric Research
(OAR) supported an instrument repair and again the SFMR returned
surface winds during the 2001 hurricane season. Since 1980, the SFMR
has flown on over 150 flights in 50 tropical cyclones.
SFMR surface winds (dashed red) and flight level winds (solid black) for
the first WP-3D pass through Hurricane Katrina on Aug 28 from northeast (left)
to southwest (right). SFMR rain rate is also shown in dotted green.
Accomplishments:
- Obtain concurrent/collocated surface wind estimates from HRD and
AOC SFMRs and GPS dropwindsondes -- Status: completed 16 missions in
3 hurricanes (Frances/Ivan/Jeanne)
-
Send report to NHC on performance of SFMR during landfalls of
Hurricanes Ivan and Jeanne -- Status:
completed Oct. 2004
- Obtain raw measurements for both SFMR systems from AOC -- Status:
completed Dec. 2004
- Post-processing of HRD SFMR measurements -- Status: completed
Jan. 2005
- Post-processing of AOC SFMR measurements -- Status:
completed Feb. 2005
- Presentation of initial results of intercomparison between HRD and
AOC SFMR wind measurements at 59th IHC -- Status: completed
March 2005
- Updated calibration for AOC SFMR and testing of alternative
calibration procedures
-- Status: completed April 2005
- Post-processing of GPS sonde surface wind estimates -- Status :
completed April 2005
Goals:
- Indentifying collocated SFMR and GPS surface wind estimates and
performing statistical analyses -- Status: Expected completion
3rd Q 2005
- Calibration flights to test results in prepartation for 2005 season
-- Status: Expected completion 3rd Q 2005
- Execute 2005 flight missions to collect additional data and
test new calibration procedures -- Status: Expected completion
4th Q 2005
- Prepare final report documenting results of evaluation report --
Status: expected completion 4th Q 2005
Key references:
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Last modified: 2/23/2005
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