Landscape variations in understory PAR for a mixed deciduous forest in New England, USA

Fladeland, M., M. S. Ashton, and X. Lee (2003), Landscape variations in understory PAR for a mixed deciduous forest in New England, USA, Agricultural and Forest Meteorology., 118, 137-141.

Summary of measurement intercomparisons during TRACE-P

Eisele, F., et al. (2003), Summary of measurement intercomparisons during TRACE-P, J. Geophys. Res., 108, 8791, doi:10.1029/2002JD003167.

Thermodynamics of crystal nucleation in multicomponent drops: The effects of surface adsorption and dissociation

Djikaev, Y., A. Tabazadeh, and H. Reiss (2003), Thermodynamics of crystal nucleation in multicomponent drops: The effects of surface adsorption and dissociation, J. Chem. Phys., 118, 6572.

and A. Tabazadeh. The effect of adsorption on the uptake of organic trace gas by cloud droplets

Djikaev, Y. (2003), and A. Tabazadeh. The effect of adsorption on the uptake of organic trace gas by cloud droplets, J. Geophys. Res., 108, 4689, doi:10.1029/2003JD003741.

Aerosol chemical composition in Asian continental outflow during the TRACE-P campaign: Comparison with PEM-West B

Snow removal and ambient temperature effects on Vermont forest soil thermal properties

Decker, et al. (2003), Snow removal and ambient temperature effects on Vermont forest soil thermal properties, Soil Science Society of America Journal, 67, 1234-1242.

Elevation and vegetation influences on soil properties in Chilean Nothofagus forests

Decker, K. L. M., and R. E. J. Boerner (2003), Elevation and vegetation influences on soil properties in Chilean Nothofagus forests, Revista Chilena de Historia Natural, 76, 371-381.

Boundary layer aerosol composition over Sierra Nevada Mountains using 9.11- and 10.59-μm continuous wave lidars and modeled backscatter from size distribution data

Clouds and trace gas distributions during TRACE-P

Crawford, J., et al. (2003), Clouds and trace gas distributions during TRACE-P, J. Geophys. Res., 108, 8818, doi:10.1029/2002JD003177.

Anhydrous nitric acid integrated cross sections: 820 to 5300 cm-1

Chackerian, C., S. W. Sharpe, and T. A. Blake (2003), Anhydrous nitric acid integrated cross sections: 820 to 5300 cm-1, J. Quant. Spectrosc. Radiat. Transfer, 82, 429-41.

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