Met Instrumentation Exam 2

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138 Terms

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What are three types of anemometers?

Cup,Vane, Ultrasonic

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What common challenges impact wind measurements?

Physical obstructions, elevation, extreme weather events (ice), high relative humidity, pressure changes

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What standards should be followed when installing wind sensors?

Height requirements, following meteorological / WMO guidelines, technical and electrical standards, true calibration (WIND VANES MUST BE ALIGNED TRUE NORTH)

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History of Wind Measuring Instruments

1450 - Leon Battista Alberta

1483- Da Vinci

1846 - J.T Romney Robinson

1892 - W. H Dines

1965- P. Minnick

1970 - A.Pfitsch

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KNOT

-reference to velocity while the distance is using nautical miles

  • was a standard unit of measurement in 1600s using a common log device

  • speed of ship was the number of knots counted

  • 1knot- 1.15mph-0.514ms^-1


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What are typical wind speeds near the surface?

  • slight breeze, gusts, sustained winds

  • 0-130 its (0-67 ms^-1)


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What are typical wind speeds in the mid-troposphere, near the jet stream?

  • 200+ its (103 ms^-1)

  • wind is a highly non-linear phenomenon


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<p>Measuring Wind: Drag Force</p>

Measuring Wind: Drag Force

  • a force acting opposite to the relative motion of any object moving with respect to a surrounding fluid

  • can also be described as resistance


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Measuring wind: Mechanical Sensors

ex - cup or propeller anemometer, wind vane

  • uses: measurement at weather station (official and home)


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Measuring wind: In-situ electronic sensors

  • ex- hot-wire anemometer

  • fast response measurements; turbulence characterization


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Measuring wind: Drifting-position sensors

  • ex- radiosonde, driftsonde, pibal

  • uses: atmospheric sounding


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Measuring wind: sensors based on impact pressure

  • ex: pitot tube

  • use: measuring airspeed of moving vehicles including aircraft


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Measuring wind: sensors that use measurements of a time shift

  • ex: ultrasonic anemometer → Passive

  • Use: modern official weather stations; research that investigates turbulence or fluxes


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Measuring wind: sensors that use measurements of a Doppler shift

  • ex: doppler radar and lidar; wind profiler

  • Use: Remote measurement of wind at a range of positions from the sensor


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<p>Does a cup anemometer spin in a different direction based on wind direction?</p>

Does a cup anemometer spin in a different direction based on wind direction?

No, a cup anemometer always spins in the same direction no matter which way the wind is blowing!

  • Does not measure direction


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Which shape has the larges drag?

  • open shapes have larger drag force


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<p>Cup Anemometers</p>

Cup Anemometers

  • mechanical rotation of the cups and the internal supporting shaft

  • rotation of the shaft can be manually determined or determined using an electrical sensors

  • Shaft rotation is equal to revolutions per minute (frequency) and is proportional to wind speed


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<p>Cup Anemometer - Optical shutter arrangement </p>

Cup Anemometer - Optical shutter arrangement

  • as the shaft rotates, a light beam between the source and electronic detector is interrupted

  • Generates a series of digital pulses at a rate which is proportional to the rotation speed


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Cup Anemometer - Reed Switch

  • as the shaft rotates an internal magnet spins closing and opening the reed switch

  • - a brief electrical current is created and measured


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Cup Anemometers: Advantages

  • simple and robust construction

  • Simplicity of speed calculation

  • Low maintenance requirements

  • Can capture a large measurement range


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Cup Anemometers: Disadvantages

  • Overspending: records average wind speeds that are too high in gusty winds

- - When the wind speed increases, the cups spin faster, but a decrease in wind of the same magnitude does not cause the cups to slow down as quickly

  • reduce the distance between the cups and the rotational axis

  • Thresholding: wind speeds greater than 1 ms^-1 are necessary to cause the cup anemometer to turn


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<p>Propellar Anemometer </p>

Propellar Anemometer

  • measures the 3 components of wind (u,v, and w)

  • the rotation speed of the propellers is proportional to the wind speed (component) perpendicular to the propeller plane

  • often used on buoys and for turbulence studies

Carbon fiber vs. Polystyrene: lighter material breaks faster

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Propeller Anemometer: Advantages

  • lightweight material have fast time responses

  • overestimation of the mean wind speed is less than cup anemometers


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Propeller Anemometer:

  • V-error: Azimuthal variations in the wind meaning the propeller is not perpendicular (or parallel) to the wind direction - underestimation to the wind speed

  • Lightweight propellors can break in high winds

  • overspeeding error


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<p>Impeller Anemometer</p>

Impeller Anemometer

  • Wind rotates the impeller, the magnet, and the shaft inducing a current through a coil

-axis of rotation parallel to the direction of the wind

-a magnet located in the impeller along with an inductor

- the rotation of impeller produces an electrical signal proportional to the wind speed

-instrument range: 0.4-35ms^-1

QUICK TIME RESPONSE


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<p>Pressure Plate Anemometers </p>

Pressure Plate Anemometers

  • deflection of a vertically hanging plate that is oriented into the mean wind direction common in 1600s

  • The deflection is proportional to the strength of the wind

non-linear response

  • A deflection of a small weight is called a telltale


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<p>Pressure Tube Anemometers </p>

Pressure Tube Anemometers

  • measures the pressure differences of static and moving (dynamic) flow

  • has directional sensitivity


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<p>Ultrasonic Anemometer </p>

Ultrasonic Anemometer

  • time it takes for ultrasound pulses to travel forward and backwards from fixed transducers

-separation of transducers are usually 10-20 cm

-soundwaves are sent at 40-100 kHz frequency

  • Dependent on temperature and humidity


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Ultrasonic Anemometer - Advantages

  • it is absolute measurement not needing calibration (except to check that the instrument parameters are specified correctly)

  • measurements do not exhibit a time lag and can be repeated frequently to resolve high-frequency to resolve high-frequency fluctuations in the wind

  • measures all three components of the wind vector and are therefore beneficial for studying turbulent mass fluxes

  • the instrument has no moving parts that require maintenance


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Ultrasonic Anemometer - Disadvantages

  • fairly expensive

  • requires more power

  • signal loss in heavy rain or wet snow


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Wind Profilers

  • similar to weather radar, but operates on a wavelength of 0.33m or 0.6m as a vertical doppler radar

-sensitive to the backscattering of turbulent structures in the water-vapor field

-measures the Doppler shift at multiple angles


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<p>Wind Vanes</p>

Wind Vanes

  • flat vertical plate attached to a horizontal arm that rotates on a vertical shaft

- the direction of the arm becomes aligned with the wind direction due to drag force and lift force

-reduction of the drag force

-static error: misalignment of vane


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Besides visually determining the direction of the vane what methods are there?

  • mechanical switch with multiple contacts distributed around the shaft

  • optical encoders giving a digital representation of measure angles

  • a precision potentiometer


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ASOS Wind Measurements

  • Prior to 2007: rotating cup anemometers and a wind vane 10 meters in height

  • Now: Sonic anemometer


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From Satellite

  • monitor cloud movements


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How is the wind speed/direction at various heights determined?

using a mix of physical instruments, remote sensing technology, and mathematics modeling

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Calibration

  • wind sensors are place in a wind tunnel with a pitot tube as the reference instrument

  • the wind tunnel must be large enough to fit the sensors and provide a uniform wind flow across the tunnel


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Exposure - Is the height of wind sensors standardized?

  • yes, by the world meteorological organization

  • 10 m in height

  • good exposure in all directions with 3km

  • obstructions should be at least 20 times the height of the obstruction from the sensor

  • show accumulation, icing, extreme temperature, high wind gust, lightning induced surges


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What are three measurement principles that are utilized for radiometric measurements?

Attenuation (thickness, absorbs, scatters, etc), Resolution, Response Time

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What are two of the basic radiation laws?

Stefan-Boltzmann Law & Wien’s Law

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What are measured errors that impact radiation sensors?

Exposure, drift, systemic errors, calibration errors

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<p>Radiation</p>

Radiation

pulses of electromagnetic energy traveling as waves and generated as electrons oscillate

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<p>Shortwave (SW)</p>

Shortwave (SW)

solar radiation


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<p>Longwave (LW)</p>

Longwave (LW)

terrestrial

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<p>Azimuth</p>

Azimuth

the angle between North, measured clockwise around the observer’s horizon, and a celestial body

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Kirchoff’s Law

good absorbers are good emitters and vice versa at peculiar wavelengths

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Stefan-Boltzmann Law

the amount of energy emitted by a body is directly proportional to the fourth power of its absolute temperature

  • sigmaT^4 = emissivity

  • Units: Wm^-2

  • (assuming perfect black body)


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Wien’s Law

hotter temperatures, shorter wavelengths

  • Lamdam = 2898/T. Units [(must)(m)]


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Planck’s Law

describes the spectral density of radiation emitted by a black body at each wavelength at a given temperature (blackbody curves)

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<p>Intensity Law</p>

Intensity Law

the amount of radiant power flux is inversely proportional to distance squared

  • Solar constant = 1379 Wm^-2

  • E=P/4pid². Units [ Wm^-2)


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Sine/Cosine Law

radiant energy striking a surface at an acute angle becomes less concentrated than direct (perpendicular) radiation

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Radiant Flux

the amount of radiation coming from a source per unit time (W)

  • sun’s radiant flux is 3.9×10^(26) W


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Radiance

radiant flux emitted by a unit area of a source or scattered by a unit area of a surface within a given solid angle (wm^-2sr^-1)

  • Sun’s radiance is 1×10^7 Wm^-2sr^-1


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Watt

Js^-1 (kgm²s^-3) - Power

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Radiant Intensity

the radiant flux leaving a point on the source, per unit solid angle of space surrounding the point in W sr^-1

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Radiant Flux Density

radiative flux per unit area W m^-2

  • flux can be negative or positive


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<p>Irradiance </p>

Irradiance

radiant flux incident on a receiving surface from all directions per unit of area surface in W m^-2

  • ALWAYS POSITIVE

  • all angles combined


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Direct Solar Radiation

radiation emitted from the solid angles of the sun, received on a surface perpendicular to the axis of the cone

  • comprised of mainly unscattered and unreflected solar radiation in Wm^-2 (1367 Wm^-2)

  • MEASURED BY A PYRHELIOMETER


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Diffuse Solar Radiation

downward scattered and reflected radiation coming from the whole hemisphere with the exception of the solid angle subtended by the sun’s disc in W m^-2

  • measured by a pyranometer in a shadow band


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Global solar radiation

solar irradiance received on a horizontal surface in W m ^-2

  • measured by a pyrometer


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What is the difference between transmitted and emitted?

Transmitted: to pass or send existing energy, light or signal THROUGH a medium

Emitted: to create and give off energy light, heat, etc NOT THROUGH a medium

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Reflection

fraction of the incident flux that is reflected by a medium

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Absorption

fraction of the incident flux that is absorbed by a medium

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<p>Transmission</p>

Transmission

fraction of the incident flux that is transmitted (passed through) by a medium

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Net Radiation (R)

R= SWD-SWU+LWD-LWU [Wm^-2]

^^^ Shortwave down, shortwave up, long wave down, long wave up

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Why might the history of radiometer be relatively new?

depending you are referring to radiometer as medical device corporation (founded in 1935) or the radiometer as a scientific instrument

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History of the Radiometer

1853- Campbell-Stokes reordered invented

1873- Crookes radiometer

1885 - Jordan Sunshine recorders invented

1893 - pyranometer and pyrheliometer is invented by Angstrom (Knutsson) and anderson

1905 - Angstrom invents the pyrgeometer


Angstrom - a constant and law of absorption (a)

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Instruments - Purpose

  • Pyrheliometer - direct solar radiation

  • Pyranometer - global solar radiation

  • Photometer - light in the visible part of the spectrum

  • Albedometer - shortwave radiation received by and reflected from a surface

  • Pyrradiometer - net radiative flux of shortwave

  • Pyrometer - terrestrial radiation

  • Pyrometer - longwave radiation emitted from a surface

  • Spectro-radioometer - specific wavelength


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What does “pyro” and “ano” and “helio” in Greek mean?

  • Pyro - fire

  • Ano - above

  • Helio - sun


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Ways radiant energy is detected

  • measure the rise of temperature of a small detecting surface

  • measure the response of a photoelectric cell

  • measure response of photochemical solution

  • MET USES FIRST TWO


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<p>Photodiode</p>

Photodiode

  • LED photodiode in circuit board (I soldered)

  • 1) Light (photons) generate electrons are attracted to the K region

  • 2) holes are attracted to the A region


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Campbell - Stokes Sunshine Recorder

  • glass sphere filled with water that focuses the sun’s rays and burns the material behind it

  • sphere was altered to be solid glass

  • Length of the scorch mark indicates daily sunlight duration

  • no scorch mark indicates clouds

  • continual scorch marks on same material makes measuring daily insolation difficult


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What does a pyranometer measure? Also, why are black and white surfaces used?

measures shortwave radiation (irradiance) (global solar radiation over a hemispheric field of view)

  • great reflector and absorbers (large for each)


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Pyranometer Theory

  • black surface with a thermopile sensor surrounded by a white plate

  • the glass bulb shields the body of the instrument from the sunshine.

||» helps isolate the measurement from external thermal interferences and weather - only reacts with pure solar radiation - glass allows solar radiation but doesn’t change anything

  • good balance arguments between the black surface and white surface


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Pyranometer Theory - Thermopile

  • converts thermal energy energy into electrical energy

  • composed of thermocouples (usually in series)

  • output voltage proportional to a local temperature difference

  • range of tens or hundreds of millivolts


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<p>Pyranometer Theory</p>

Pyranometer Theory

Look at the parts

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<p>Pyranometer Theory - S equation</p>

Pyranometer Theory - S equation

Look at the equation

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Eppley Black and White Pyranometer

  • measures global solar radiation

  • reference instrument in calibration procedures of pyranometers

  • the detectors consists of three white and three black wedges representing the cold (white) and hot junctions (black) of an electroplated copper-constantan thermopile

  • can be inverted to measure albedo

  • (double domes are used to protect the instrument from the weather and a second to isolate the receiving surface from local heating)


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Why is albedo important?

Tells us urban heat island, tells us about energy balance

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<p>Albedometer</p>

Albedometer

  • measures shortwave radiation using a pair of pyrometers

  • specifically measures shortwave radiation received by and reflected from a surface

  • measurements are poor around sunset and sunrise - sun is at lower angle

Large change in albedo?

  • snow, cloud coverage, knocked down forest into parking lot


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<p>Which line is which?</p>

Which line is which?

Bottom - Su (shortwave up)

Top - Sg (shortwave down)

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<p>Pyrheliometer</p>

Pyrheliometer

  • measures direct shortwave radiation

  • specially, the measurement of direct solar radiation, normal to the solar beam

  • has a thermocouple sensor

  • a solar tracking instrument is needed- follows the sun in elevation and azimuth


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Photometer

  • measures shortwave radiation

  • specially measures light in the visible part of the spectrum only as energy

  • convert light into electricity using a photoresistor, photodiode (resistance down, intensity up), photomultiplier (amplifies the light, very sensitive)

  • light might be passed through a filter to measure at a defined wavelength


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Diffuse Solar Radiation Measurement

  • the pyranometer sensors is shaded from the direct solar beam

  • the shade ring must be regularly adjusted

  • some of the diffuse radiation is lost by the obstruction of the ring itself

  • depends on latitude and time of year

  • can be corrected by multiplying the measure value by the k factor


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<p>Look at this</p>

Look at this

“f” is the geometric factor and q is the anisotropy factor (sky cover factor)

  • width to radius ration

  • hour angle for sunset

  • solar declination


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<p>SW+LW - Pyrrandiometer Theory</p>

SW+LW - Pyrrandiometer Theory

knowt flashcard image
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Pyrradiometer

  • measures total global radiation (shortwave and long wave)

  • glass domes are not used for pyrradiometers

polytene or sillicon domes are transparent to a large range of wavelengths

  • sillicon degrades in sunlight becoming brittle, and needs to be replaced monthly


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Pyrradiometer vs. pyrometer

  • pyrometer doesn’t care about shortwave radiation


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<p>Net Pyrradiometer (radiometer)</p>

Net Pyrradiometer (radiometer)

  • measures shortwave and long wave radiation

  • specifically measures the net radiative flux of shortwave and long wave radiation


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<p>Pyrgeometer </p>

Pyrgeometer

  • measures long wave only

  • specially, measure the terrestrial radiation usually over a hemisphere, either upward or downward

  • measurements are made at night or during the day if the shortwave amount is independently measured and subtracted


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Pyrometer - Infrared Thermometer

  • measures the long wave radiation emitted in the 7.5-13.5 (mu m)

  • radiation received is related to the temperature of the surface

  • Emmistitivty = sigmat^4

  • a thermopile sensing element, composed of small thermocouples on a sillicon chip, absorb the energy and produce an output signal


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ASOS Radiometer

  • no radiometers at the ASOS stations

  • NYS Mesonet: Li-Cor Pyranometer:

weather resistant and durable in long-term outdoor deployments

measures global solar radiation under unobstructed natural daylight conditions

uniform sensitivity u to 82 degrees incident angle

detachable sensor simplifies installation and removal, making it ideal for platforms with complex cabling


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Radiometers and Satellites

  • radiometers flown on satellites are NOT cameras

  • moving mirror make the radiometer view different regions of the earth

  • radiometer scans a scene line-by-line

  • data is recorded in a two-dimensional format (line and element) which, when displayed on a computer monitor or television screen, makes up an image


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Radiometers on a satellite is a…

Passive sensors

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Radiometric resoultion

  • the number of bits representing the recorded energy

  • 8-bit: 256 values (2^8)

  • 4-bit: 16 values (2^4)

  • 1-bit: 1 value (0 or 1)


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Spectral Resoultion

  • the greater the number of bands, the greater the spectral resolution


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Spatial Resolution

  • the size of a pixel that is recorded in a raster image, typically pixels may correspond to square areas ranging in side length from 1 to 1000m

  • very expensive


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Temporal Resolution

  • geostationary orbit

  • near polar-orbit

  • sun-synchronous orbit


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Measurement Error: Azimuth Error

  • change in the sensors output as the sensor is rotated about the normal axis at a particular angle of incident radiation


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Measurement Error: Linearity Error

the sensor output is not linearly proportional to the input