Jens Redemann 1 , B. Schmid 1 , J. M. Livingston 2 , P. B. Russell 3 , J. E. Eilers 3 ,
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Transcript of Jens Redemann 1 , B. Schmid 1 , J. M. Livingston 2 , P. B. Russell 3 , J. E. Eilers 3 ,
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Airborne Sunphotometry in Support of the Airborne Sunphotometry in Support of the Chesapeake Lighthouse and Aircraft Measurements Chesapeake Lighthouse and Aircraft Measurements
for Satellites (CLAMS) Experiment, 2001for Satellites (CLAMS) Experiment, 2001
Jens RedemannJens Redemann11, B. Schmid, B. Schmid11, J. M. Livingston, J. M. Livingston22, P. B. Russell, P. B. Russell33, J. E. Eilers, J. E. Eilers33, , P. V. HobbsP. V. Hobbs44, R. Kahn, R. Kahn55, W. L. Smith Jr., W. L. Smith Jr.66,, B. HolbenB. Holben7 7 , K. Rutledge, K. Rutledge88
11Bay Area Environmental Research Institute, CABay Area Environmental Research Institute, CA22SRI International, CA, SRI International, CA, 33NASA Ames Research Center, CA NASA Ames Research Center, CA 44University of Washington, WA, University of Washington, WA, 55Jet Propulsion Lab, CAJet Propulsion Lab, CA
66NASA LaRC, VA, NASA LaRC, VA, 77NASA GSFC, MD, NASA GSFC, MD, 88AS&M, Inc./NASA LaRC, VAAS&M, Inc./NASA LaRC, VA
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ContentsContents1.1. Purpose of CLAMSPurpose of CLAMS2.2. Sunphotometer measurements aboard the Sunphotometer measurements aboard the
UW CV-580 – comparability with other UW CV-580 – comparability with other platforms and instrumentsplatforms and instruments
3.3. Comparisons of AATS-14 to AERONET Cimel Comparisons of AATS-14 to AERONET Cimel sunphotometer at COVEsunphotometer at COVE
4.4. First validation attempts of the MISR First validation attempts of the MISR standard algorithmstandard algorithm
5.5. Spatial statistics of AOD off the US East Spatial statistics of AOD off the US East CoastCoast
6.6. ConclusionsConclusions
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Chesapeake Lighthouse: Centerpiece of CLAMS observationsChesapeake Lighthouse: Centerpiece of CLAMS observations
• CLAMS: clear sky, shortwave (SW) closure campaign
• CERES, MISR, MODIS-Atmospheres, and the NASA/GEWEX/GACP
• Measurements from:A. Chesapeake Lighthouse research
platform (36.9N,75.7W), B. 6 research aircraft,C. TERRA satellite • CLAMS research goals: A. validation of satellite-based
retrievals of aerosol properties, B. vertical profiles of radiative
fluxes, C. temperature and water vapor
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AATS-14 aboard the UW CV-580AATS-14 aboard the UW CV-580
1. Measures direct solar beam transmission @:353.5 380.0 449.0 499.4 525.0 605.7 675.1 778.4 864.5 939.7 1019.1 1059.4 1241.3 1557.8 nm
2. Yields:aerosol optical depth + aerosol extinction when A/C flies profiles
columnar water vapor (ozone) + water vapor (ozone) concentration when A/C flies profiles
3. Size:Telescope dome 8" OD (hemisphere) atop 5" H pedestal. (Total H: 9" above A/C skin), Inside A/C: 12" D x 18" H cylinder.
4. Weight:131.6 lbs
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Typical Typical UW CV-580 UW CV-580 flight track in flight track in
CLAMSCLAMS
Chesapeake Lighthouse
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Typical AATS-14 measurement dayTypical AATS-14 measurement day
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AERONET vs. AATS-14 at COVE, July 17, 2001AERONET vs. AATS-14 at COVE, July 17, 2001
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Statistics of AERONET vs. AATS-14 at COVE, July 10 – Aug.2, 2001Statistics of AERONET vs. AATS-14 at COVE, July 10 – Aug.2, 2001
y=1.035x+0.016r2=0.995rmse=0.04
y=1.041x+0.002r2=0.993rmse=0.021
y=0.987x-0.004r2=0.959rmse=0.011
y=0.957x-0.005r2=0.916rmse=0.012
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CV-580/AATS-14 location, CLAMS July 17, 2001, CV-580/AATS-14 location, CLAMS July 17, 2001, 16:00 - 16:15 UTC16:00 - 16:15 UTC
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AOD variability on July 17AOD variability on July 17thth, 2001, 2001
ΔAOD~25%
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Comparison between AATS-14, AERONET and MISR (unvalidated Comparison between AATS-14, AERONET and MISR (unvalidated standard algorithm), CLAMS, July 17, 2001standard algorithm), CLAMS, July 17, 2001
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Vertical aerosol structure, July 17, 2001Vertical aerosol structure, July 17, 2001
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ConclusionsConclusions1. In CLAMS, AATS-14 measured full column aerosol optical depth
spectra and columnar water vapor at exact TERRA overpass time on at least 7 occasions.
2. For five of these opportunities, AOD at 499nm was at or below 0.1.
3. During TERRA overpass time on July 17, 2001, AATS-14 measured the highest AOD encountered during the entire experiment (~0.48 at 499nm), including a horizontal gradient in AOD of more than 0.1 over a horizontal distance of ~80 kilometers.
4. Comparisons between airborne AATS-14 in the vicinity of and AERONET Cimel derived AOD’s directly at the Chesapeake Lighthouse show good agreement (and strongest correlation coefficients at 380 and 500 nm).
5. Initial validation studies of the standard MISR AOD algorithm seem to indicate the lack of small particles in the mixture models.
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AcknowledgmentAcknowledgment
We gratefully acknowledge funding for We gratefully acknowledge funding for AATS-14 participation in CLAMS through AATS-14 participation in CLAMS through the EOS Validation Program (M. King).the EOS Validation Program (M. King).