Hygroscopicity and chemical composition of Antarctic sub-micrometre aerosol particles and observations of new particle formation
Texto
Imagem
Documentos relacionados
As an initial application of the κ -based lookup tables, and to test the role of the parti- cle size distribution and aerosol hygroscopicity, sensitivity simulations were carried
Aircraft – based measurements of aerosol hygroscopicity, both in the form of size- resolved, diameter growth factors and in the dependence of particle light scattering on
We then summarize airborne measurements, made in the troposphere of the Alaskan Arctic, of aerosol particle size distributions, composition, and optical proper- ties and discuss
Fine particle nucleation over MeJA-treated cabbage plants (cvs. Lennox and Rinda): (a) a contour plot of aerosol particle number size distributions (measured with the DMPS), (b)
Free amino acids in Antarctic aerosol: potential markers for the evolution and fate of marine aerosol..
Investigating the formation of particle volume in the summer Central Antarctic base- line aerosol further, an annual cycle in the total particle volume in these air masses is
Both the ability of an aerosol particle to act as a CCN at a given S level and its contribution to extinction depends on the aerosol particle size distribution. Particle size is
P ¨oschl, U.: Aerosol- and updraft-limited regimes of cloud droplet formation: influence of par- ticle number, size and hygroscopicity on the activation of cloud condensation