@article{
 title = {Particle nucleation in the tropical boundary layer and its coupling to marine sulfur sources},
 type = {article},
 year = {1998},
 keywords = {Cloud condensation nuclei,aerosol-size distribution,atmospheric sulfur,cycles,dimethyl sulfide,entrainment,ocean,pacific,saga-3,sulfate},
 pages = {89-92},
 volume = {282},
 id = {52e7414d-fb0e-34a1-8967-3120155333c9},
 created = {2015-05-08T02:34:10.000Z},
 file_attached = {true},
 profile_id = {f8c267c4-4c39-31dc-80fa-3a9691373386},
 group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
 last_modified = {2015-05-08T12:55:28.000Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 source_type = {Journal Article},
 notes = {Article},
 abstract = {New particle formation in a tropical marine boundary Layer setting was characterized during NASA's Pacific Exploratory Mission-Tropics A program. It represents the clearest demonstration to date of aerosol nucleation and growth being Linked to the natural marine sulfur cycle. This conclusion was based on real-time observations of dimethylsulfide, sulfur dioxide, sulfuric acid (gas), hydroxide, ozone, temperature, relative humidity, aerosol size and number distribution, and total aerosol surface area. Classic binary nucleation theory predicts no nucleation under the observed marine boundary layer conditions.},
 bibtype = {article},
 author = {Clarke, A D and Davis, D and Kapustin, V N and Eisele, F and Chen, G and Paluch, I and Lenschow, D and Bandy, A R and Thornton, D and Moore, K and Mauldin, L and Tanner, D and Litchy, M and Carroll, M A and Collins, J and Albercook, C},
 journal = {Science},
 number = {5386}
}

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