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Aerosol concentrations and 3-D winds were measured from September 9 to 25, 2007, above a pine forest in California. The measurements were combined using the eddy covariance (EC) technique to determine aerosol eddy fluxes as a function of particle diameter within the accumulation mode size range (0.25 µm ≤ D p ≤ 1 µm here). Measured heat and water vapor fluxes were utilized to correct the aerosol eddy fluxes for aerosol hygroscopic growth. The hygroscopic growth correction was necessary despitedoi:10.5194/acp-10-5749-2010 fatcat:jycexnigojbdrc4iqfdo5kyvmu