atmospheric sciences 370 observing systems winter 2013

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Atmospheric Sciences 370 Observing Systems Winter 2013

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Atmospheric Sciences 370 Observing Systems Winter 2013. ASOS: Automated Surface Observing System: Backbone Observing System in the U.S. ASOS. Located at primary and secondary airports Sponsored by the FAA and NWS High quality instrumentation that is well maintained and calibrated. - PowerPoint PPT Presentation

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Page 1: Atmospheric Sciences 370 Observing Systems Winter 2013

Atmospheric Sciences 370 Observing Systems

Winter 2013

Page 2: Atmospheric Sciences 370 Observing Systems Winter 2013

ASOS: Automated Surface Observing System:

Backbone Observing System in the U.S.

Page 3: Atmospheric Sciences 370 Observing Systems Winter 2013

ASOS• Located at primary and secondary airports• Sponsored by the FAA and NWS• High quality instrumentation that is well

maintained and calibrated.• Reported in METAR format (more later)

Page 4: Atmospheric Sciences 370 Observing Systems Winter 2013

Hydrothermograph

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Precipitation Gauges

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Laser WeatherIdentifier

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Acoustic Anemometer

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AnemometerWind Vane

Still used in many systems

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Laser Ceilometer

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The ASOS Freezing Rain Sensor

uses an ultrasonically vibrating probe to detect the presence of icing conditions. The vibrating frequency of the probe decreases with the accumulation of ice.

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Lightning SensorVisibility Sensor

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Full ASOS system in Arizona

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METAR Format• ASOS data (and airport observations worldwide) are

transmitted in METAR format.• Name came from the French words, MÉTéorologique

("Weather") Aviation Régulière ("Routine").• Example: KSEA 042353Z 11008KT 10SM FEW050

SCT070 OVC090 09/03 A2879 RMK AO2 SLP756 60001 T00940033 10117 20083 58013

• Will learn more about it in Lab

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Observing Heights (ASOS and most official obs)

• Temperature and dew point (2-m)• Wind speed and direction (10-m)

Page 15: Atmospheric Sciences 370 Observing Systems Winter 2013

Other Surface Networks•Bureau of Land Management•RAWS•Agrimet•PAWS•Department of Ecology•Puget Sound Clean Air•BC Hydro•BC Olympics•Weather Underground•Many more!

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NWNet: Regional Real-Time Collection of Over 70 Networks Over the Pacific Northwest

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Oklahoma Mesonet

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Networks of Networks

UW: We collect data from about 70 networks in real time over NW

Mesowest: Collects about 100 networks over the western third of U.S.

Madis: national collection of mesonets

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Marine Reports

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Ocean and LakeWeather Buoys

Anchored

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Drifting Buoys

Wind Pressure

Page 23: Atmospheric Sciences 370 Observing Systems Winter 2013

Coastal Marine (CMAN) Reports from the Coast Guard

Page 24: Atmospheric Sciences 370 Observing Systems Winter 2013

Northwest Buoy and CMAN Locations

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Ship Reports: Marine VOS Program

Volunteers Observers--generally 6-hourly reportsHighly variable quality and frequency

Page 27: Atmospheric Sciences 370 Observing Systems Winter 2013

SatelliteMicrowaveScatterometerWinds

Page 28: Atmospheric Sciences 370 Observing Systems Winter 2013

QuickScat SatelliteBounces microwaves off the ocean surfaceCapillary waves dependent on wind speed and directon

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Upper Air Data

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Radiosonde

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Radar Wind Profiler and RASS (Radio Acoustic Sounding System)

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Seattle Profiler/RASS

Page 36: Atmospheric Sciences 370 Observing Systems Winter 2013

Profiler Locations

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ACARS: Aircraft ObservationsGenerally on wide-body aircraft

Aircraft Communications Addressing and Reporting System

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New Satellite Observing Capabilities

Page 42: Atmospheric Sciences 370 Observing Systems Winter 2013

Cloud andWater VaporTrack WindsBased on Geostationary Weather Satellites

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Satellite Temperature and Humidity Soundings

Page 45: Atmospheric Sciences 370 Observing Systems Winter 2013

GOES sounder unit

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GPS Sounding

• A constellation of GPS satellites orbit the earth.• A collection of other satellites can receive the GPS

signal• By measuring the delay in time as the GPS signal is

bent by the earth’s atmosphere, one can acquire density information that can be used to create temperature and humidity soundings.

• Can do this with fixed receivers on earth or with receivers on satellites--the COSMIC project.

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Typical Observation Errors at the Surface

(Important when doing analyses!)• Sea Level Pressure

– Low-Elevation land stations +-.5 mb– Ships +- 1-5 mb

• Temperature: +-1C• Wind Speed: +-2-5 knots, very light winds often

a problem—especially for classical anomemters.• Relative Humidity: +-10%

Page 51: Atmospheric Sciences 370 Observing Systems Winter 2013

Typical Radiosonde Errors

• Geopotential heights: – 700 mb (hPa): 5-10 m– 500 mb 10-15 m– 300 mb 15-20 m– 100 mb 20-30 m

• Temperature: +-0.5C• Wind speed: +-5%,+-10 degrees

Page 52: Atmospheric Sciences 370 Observing Systems Winter 2013

Terminology• Direct versus Indirect observations

– Direct: measurement at the location of the instrument

– Indirect: remotely sensed using radiation measurements

• Active versus passive remote sensing– Active: instrument emits radiation, analyzes return– Passive: analyzes incoming natural radiation