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Wiley InterScience

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Regional aerosol optical depth characteristics from satellite observations: ACE‐1, TARFOX and ACE‐2 results
P. A. Durkee 1 , K. E. Nielsen 1 , P. J. Smith 1 , P. B. Russell 2 , B. Schmid 3 , J. M. Livingston 4 , B. N. Holben 9 , C. Tomasi 11 , V. Vitale 11 , D. Collins 5 , R. C. Flagan 5 , J. H. Seinfeld 5 , K. J. Noone 6 , E. Öström 9 , S. Gassó 7 , D. Hegg 7 , L. M. Russell 10 , T. S. Bates 8 and P. K. Quinn 8 ,
  1 Naval Postgraduate School, Monterey, CA USA;   2 NASA Ames Research Center, Moffett Field, CA USA;   3 Bay Area Environmental Research Institute, San Francisco, CA 94122, USA;   4 SRI International, Menlo Park, CA 94025, USA;   5 California Institute of Technology, Pasadena, CA, USA;   6 Stockholm University, Stockholm, Sweden;   7 University of Washington, Seattle, WA, USA;   8 NOAA PMEL, Seattle, WA, USA;   9 NASA Goddard Space Flight Center, Greenbelt, MD, USA;   10 Princeton University, Princeton, NJ, USA;   11 FISBAT, Bologna, Italy
Corresponding author: 589 Dyer Road, Room 254,
Monterey, CA, 93943–5113, USA.
e‐mail: Durkee@nps.navy.mil.
Copyright © Munksgaard 2000

ABSTRACT

Analysis of the aerosol properties during 3 recent international field campaigns (ACE‐1, TARFOX and ACE‐2) are described using satellite retrievals from NOAA AVHRR data. Validation of the satellite retrieval procedure is performed with airborne, shipboard, and land‐based sunphotometry during ACE‐2. The intercomparison between satellite and surface optical depths has a correlation coefficient of 0.93 for 630 nm wavelength and 0.92 for 860 nm wavelength. The standard error of estimate is 0.025 for 630 nm wavelength and 0.023 for 860 nm wavelength. Regional aerosol properties are examined in composite analysis of aerosol optical properties from the ACE‐1, TARFOX and ACE‐2 regions. ACE‐1 and ACE‐2 regions have strong modes in the distribution of optical depth around 0.1, but the ACE‐2 tails toward higher values yielding an average of 0.16 consistent with pollution and dust aerosol intrusions. The TARFOX region has a noticeable mode of 0.2, but has significant spread of aerosol optical depth values consistent with the varied continental aerosol constituents off the eastern North American Coast.


Received 9 February 1999; in final form 6 September 1999

DIGITAL OBJECT IDENTIFIER (DOI)
10.1034/j.1600-0889.2000.00040.x About DOI

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