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Technology Today Volumn 3 Issue 1 - Raytheon

Technology Today Volumn 3 Issue 1 - Raytheon

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SATELLITE Sensors<br />

Space-borne Microwave<br />

Remote Sensing<br />

Microwave remote sensing has evolved into<br />

an important all-weather tool for monitoring<br />

the atmosphere and planetary object<br />

surfaces, which emphasizes the characterization<br />

of the earth phenomenology. This<br />

type of sensing encompasses the physics of<br />

radio wave propagation and interaction<br />

with material media, including surface and<br />

volume scattering and emissions. “Active”<br />

remote sensors include scatterometers,<br />

Synthetic Aperture Radar (SAR) and altimeters,<br />

whereas “passive” sensors are known<br />

as microwave radiometers. <strong>Raytheon</strong> has<br />

a 30-plus-year history in space Satellite<br />

Communications (SATCOM) and within the<br />

last decade, has added remote sensing payloads<br />

to our repertoire of outstanding<br />

orbital performances.<br />

The SeaWinds remote sensor has a specialized<br />

Ku-band radar (scatterometer),<br />

designed to accurately measure the amplitude<br />

scattering return from the ocean and<br />

convert the data into global ocean surface<br />

wind speeds and directions. A normalized<br />

radar backscatter coefficient of the ocean<br />

surface is measured at the same point on<br />

the ocean surface at four different incident<br />

angles, and is a function of the angle of<br />

incidence and the sea state. Receive power<br />

is determined by measuring the power in<br />

narrow- and wide-band filters, then solving<br />

two simultaneous equations from the<br />

received power and the ubiquitous receiver<br />

noise. The science community experimentally<br />

and analytically established a geophysical<br />

model of wind vectors and wind geometry<br />

over the last two decades to achieve<br />

this complex indirect measurement from<br />

space. The Scatterometer Electronic<br />

Subsystem (SES) was designed and developed<br />

by <strong>Raytheon</strong> St. Petersberg for the<br />

NASA/JPL program, and is currently on orbit<br />

and fully operational. Examples of previous<br />

wind vector maps of the Atlantic and<br />

Pacific oceans and newly acquired data<br />

from QuikScat’s SeaWinds are shown in the<br />

figure (center column). The radar operates<br />

at a carrier frequency of 13.402 GHz with a<br />

10<br />

nominal peak power of 110 watts, pulse<br />

rate of 192 Hz and pulse width of 1.5<br />

m/sec. The highly stable receiver measures<br />

the return echo power from the ocean to a<br />

precision of 0.15 dB. Key measurements<br />

are a 1,800 km swath during each orbit<br />

providing 90 percent coverage of the<br />

Earth’s oceans every day, with wind speed<br />

measurement range from 3 to 30 m/sec<br />

with a 2 m/sec accuracy and wind direction<br />

accuracy of 20 degrees at a vector resolution<br />

of 25 km.<br />

Fifteen times a day, the satellite beams<br />

collected science data to NASA ground stations,<br />

which relay the data to scientists and<br />

weather forecasters. Winds play a major<br />

role in weather systems and directly affect<br />

the turbulent exchanges of heat, moisture<br />

and greenhouse gases between the Earth’s<br />

atmosphere and the ocean. They also play<br />

a crucial part in the scientific equation for<br />

determining long-term climate change.<br />

Data from SeaWinds’ two-year mission will<br />

greatly improve meteorologists’ ability to<br />

forecast weather and understand longerterm<br />

climate change. SeaWinds provides<br />

ocean wind coverage to an international<br />

team of climate specialists, oceanographers<br />

and meteorologists interested in discovering<br />

the secrets of climate patterns and improving<br />

the speed with which emergency preparedness<br />

agencies can respond to fastmoving<br />

weather fronts, floods, hurricanes,<br />

tsunamis and other natural disasters.<br />

Operating as NASA’s next<br />

El Nino watcher,<br />

QuikScat will be<br />

used to better<br />

understand<br />

global El Nino<br />

and La Nina weather abnormalities. A<br />

recent example of the advantages of spaceborne<br />

sensing was demonstrated when an<br />

iceberg the size of Rhode Island had elluded<br />

ship-borne and airborne surveillance<br />

devices and was drifting undetected off<br />

Antarctica until Quikscat located it and<br />

mapped its location (see figure above).<br />

Another on-orbit remote sensor is the US<br />

Navy GeoSAT Follow-On Ku-Band Radar<br />

Altimeter, designed to maintain continuous<br />

ocean observation from the GFO Exact<br />

Repeat Orbit. This satellite includes all the<br />

capabilities necessary for precise measurement<br />

of both mesoscale and basin-scale<br />

oceanography. Data retrieved from this<br />

satellite is useful for ocean research, offshore<br />

energy production, ocean circulation<br />

patterns and environmental change. GFO<br />

was launched aboard a TAURUS launch<br />

vehicle on Feb. 10, 1998, from Vandenberg<br />

Air Force Base in California and still provides<br />

valuable data sets for the U.S. Navy<br />

today. The radar uses co-boresighted<br />

radiometers, a <strong>Raytheon</strong> design, for water<br />

vapor correction. Radiometer calibration<br />

has become a niche area of research, and<br />

<strong>Raytheon</strong> holds several patents in calibrating<br />

radiometers using variable Cold Noise<br />

Sources based on MHEMT technology that<br />

have been validated at NIST.<br />

Space-borne SATCOM<br />

Payloads<br />

From Iridium to MILSTAR to FLTSATCOM,<br />

<strong>Raytheon</strong> has played a key role in the<br />

development of commercial military space<br />

satellite communications. <strong>Raytheon</strong> is the<br />

major supplier of UHF SATCOM products<br />

and services to the warfighter, including<br />

space and ground hardware, software,<br />

Continued on page 30

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