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Published byAgnes Lane Modified over 9 years ago
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The A-Train: Exploiting the Electromagnetic Spectrum
Chip Trepte NASA Langley Research Center
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What is the A-Train? Constellation of satellites flying in formation to observe the same area and almost the same time but with using different techniques Orbit crosses equator around 1:30 pm local time or in the ‘Afternoon’ and (originally) lead by the Aqua mission Named after the ‘Take the A-Train’ jazz tune composed by Billy Stayhorn and made popular by Duke Ellington’s band. Data collected synchronously gives more- complete answers to important scientific questions than would be possible with observations collected at different times
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A-Train Members Mission Instruments Purpose Aqua (2002) CALIPSO (2006)
AIRS, AMSR-E, AMSU-A, CERES, HSB, MODIS Clouds, temperature, moisture, precipitation, ice, snow, reflected radiation and Earth emitted radiation, sea surface temperature CALIPSO (2006) CALIOP, IIR, WFC Profiles of aerosols and clouds, IR properties of clouds CloudSat (2006) CPR Profiles of cloud water amount Aura (2004) HIRDLS, MLS, OMI, TES Composition and temperature of upper atmosphere GCOM-W (2012) AMSR2 Precipitation, relative humidity, temperature
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A-Train Instrument Techniques
Mission Instruments Aqua (2002) AIRS (IR sensor) AMSR-E, AMSU-A (microwave sensor) CERES (visible/IR sensor) HSB (microwave sensor) MODIS (visible/IR sensor) CALIPSO (2006) CALIOP (active lidar) IIR (IR sensor) WFC (visible sensor) CloudSat (2006) CPR ( active radar) Aura (2004) HIRDLS (IR sensor) MLS (microwave sensor) OMI (visible sensor) TES (IR sensor) GCOM-W (2012) AMSR2 (microwave sensor)
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Basic Properties of Light
Electromagnetic radiation propagates as a wave oscillating electric and magnetic fields theory provided by James Clerk Maxwell (1865) Three primary characteristics intensity (amplitude of wave) color (wavelength or frequency of wave) polarity (propagation plane of wave)
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Electromagnetic Spectrum
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Attenuation of Light Transmission of light through a substance is affected by the absorption and scattering of light. August Beer (1854), Johann Lambert (1760) discovered this relationship
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Emission of Light Objects of different temperatures emit light that peak at different wavelengths Hotter objects emits most radiation at shorter wavelengths Cooler objects emit most radiation at longer wavelengths Discovered by Wilhelm Wien (1893)
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Possible interactions between photons and molecules/atoms
Visible and UV light: changes electron distribution in orbits (orbit transitions) Infrared light: changes vibration/rotation states Microwave light: changes rotation states
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Earth’s Atmosphere Limb View of Atmosphere:
Troposphere – orange/yellow shades and contains > 80% of mass and holds almost all water and clouds Stratosphere – pinkish hue and where ozone layer exists Mesosphere and above – blueish hues
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Atmosphere Composition
Gas Percent Volume Nitrogen 78.084% Oxygen 20.946% Argon 0.9340% Carbon dioxide % Neon % Helium % Methane % Krypton % Hydrogen % Nitrous oxide % Carbon monoxide % Xenon % Ozone % Water Vapor ~0.4% (1-4% at surface)
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Atmospheric Aerosols/Particles
Particles or Aerosols are present throughout the atmosphere pollen, dust, smoke ash, rain or sulphuric acid droplets ice and snow crystals …… Composed of many substances water, ice, water/ice, soluble gases, carbon cores … Scatter light in many ways geometric optics (rainbows, halos Rayleigh (molecular) scattering Mie scattering Range in size 6 or 8 orders of magnitude (.01 microns to 10 cm) Gustav Mie Lord Rayleigh
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Techniques for Remote Sensing
Detector Detector Light source Emission atmosphere Transmission Detector Source Detector Scattering from incoherent source Scattering from coherent source (Active Remote Sensing)
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CALIOP - aerosol altitude, phase/type
Exploiting A-Train synergy for volcanic cloud studies Aura Aqua OMI - SO2, ash, BrO TES - SO2 MLS - UTLS SO2, HCl, IWC MODIS - SO2, ash, sulfate, ice AIRS - SO2, ash, sulfate, ice, SO2 profile CloudSat CALIPSO CPR – precipitation, hydrometeors CALIOP - aerosol altitude, phase/type The A-Train
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Soufrière Hills volcano (Montserrat) eruption, May 2006
~0.2 Tg SO2 [Carn et al., 2007; Prata et al., 2007]
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Soufrière Hills volcano (Montserrat) eruption, May 2006
~0.2 Tg SO2 [Carn et al., 2007; Prata et al., 2007]
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Soufrière Hills volcano (Montserrat) eruption, May 2006
~0.2 Tg SO2 [Carn et al., 2007; Prata et al., 2007]
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Soufrière Hills volcano (Montserrat) eruption, May 2006
~0.2 Tg SO2 [Carn et al., 2007; Prata et al., 2007]
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CALIPSO first light – 7 June 2006
OMI SO2 – 7 June 2006 OMI SO2 - 7 June 2006 CALIPSO ‘first light’ - 7 June 2006
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Clear air in Beijing Aqua-MODIS RGB October
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Hazardous air in Beijing
MODIS-RGB October
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MODIS-RGB + Aura- OMI SO2 October 8 2010
SO2 pollution from coal burning Power Plants and industries (metal smelting)
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Combined CALIPSO/CloudSat Cloud Observations
“Great Arc Cloud” MODIS 12 µm (Channel 32)
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CALIPSO 532 nm Backscatter
Height 15 10 5 CALIPSO 532 nm Backscatter Height 15 10 5 CALIPSO 1064 nm Backscatter Height 15 10 5 CloudSat Cloud Mask Height 15 10 5 CloudSat Radar Reflectivity (dBZ)
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Aerosol and Cloud Observations over Southern Asia
MODIS only October 25, 2006
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Aerosol and Cloud Observations over Southern Asia
CALIPSO and MODIS October 25, 2006
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