<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lin, P.</style></author><author><style face="normal" font="default" size="100%">Hu, M.</style></author><author><style face="normal" font="default" size="100%">Wu, Z.</style></author><author><style face="normal" font="default" size="100%">Niu, Y.</style></author><author><style face="normal" font="default" size="100%">T. Zhu</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Marine aerosol size distributions in the springtime over China adjacent seas</style></title><secondary-title><style face="normal" font="default" size="100%">Atmospheric Environment</style></secondary-title><alt-title><style face="normal" font="default" size="100%">Atmos. Environ.</style></alt-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">air</style></keyword><keyword><style  face="normal" font="default" size="100%">atlantic</style></keyword><keyword><style  face="normal" font="default" size="100%">boundary-layer aerosol</style></keyword><keyword><style  face="normal" font="default" size="100%">china adjacent</style></keyword><keyword><style  face="normal" font="default" size="100%">emissions</style></keyword><keyword><style  face="normal" font="default" size="100%">Environmental Sciences &amp; Ecology</style></keyword><keyword><style  face="normal" font="default" size="100%">experiment ace 1</style></keyword><keyword><style  face="normal" font="default" size="100%">marine aerosol</style></keyword><keyword><style  face="normal" font="default" size="100%">Meteorology &amp; Atmospheric Sciences</style></keyword><keyword><style  face="normal" font="default" size="100%">nonprecipitating clouds</style></keyword><keyword><style  face="normal" font="default" size="100%">number</style></keyword><keyword><style  face="normal" font="default" size="100%">number concentration</style></keyword><keyword><style  face="normal" font="default" size="100%">pacific</style></keyword><keyword><style  face="normal" font="default" size="100%">particles</style></keyword><keyword><style  face="normal" font="default" size="100%">physical-properties</style></keyword><keyword><style  face="normal" font="default" size="100%">seas</style></keyword><keyword><style  face="normal" font="default" size="100%">size distribution</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2007</style></year><pub-dates><date><style  face="normal" font="default" size="100%">Oct</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">32</style></number><volume><style face="normal" font="default" size="100%">41</style></volume><pages><style face="normal" font="default" size="100%">6784-6796</style></pages><isbn><style face="normal" font="default" size="100%">1352-2310</style></isbn><language><style face="normal" font="default" size="100%">English</style></language><abstract><style face="normal" font="default" size="100%">Size distributions and particle number concentrations of atmospheric aerosols in the size (diameter) range from 15 mn to 10 mu m were measured on board of a research ship during three cruises in China adjacent seas. The total particle number concentrations were in average around 4000 cm(-3) in Yellow Sea, 2000 cm(-3) in East China Sea and 1000 cm(-3) in South China Sea. The observed size distributions were fitted with two or three log-normal modes and the data were classified according to time, regions and calculated air mass back-trajectories. The size distribution spectra of air masses of polluted continental origin as their back-trajectories showed were characterized by single mode with total number concentrations between 1000 and 10000 cm(-3). The size distributions in marine air masses showed dual mode characteristics, one maximum at 40-60 nm and the other at 160-190 nm with total number concentrations below 1000 cm(-3). This type of dual mode was more pronounced at longer residence time of the air masses over the ocean. The burst of ultra-fine (UF) particles and the consequent growth processes were observed twice in Yellow Sea and possible reasons leading to these events are discussed. The particle growth rate (GR) was 3.4 +/- 0.9 and 3.5 +/- 1.6 nm h(-1), respectively (95% confidence interval), indicating that the UF particles can grow to cloud condensation nuclei (CCN) within the next 1-2 days.) (C) 2007 Elsevier Ltd. All rights reserved.</style></abstract><work-type><style face="normal" font="default" size="100%">Article</style></work-type><accession-num><style face="normal" font="default" size="100%">WOS:000250489600009</style></accession-num><notes><style face="normal" font="default" size="100%">ISI Document Delivery No.: 225ANTimes Cited: 21Cited Reference Count: 37Lin, Peng Hu, Min Wu, Zhijun Niu, Yuwen Zhu, TongWu, Zhijun/A-7041-2012; ZHU, TONG/H-6501-2011; Lin, Peng/G-4867-2016ZHU, TONG/0000-0002-2752-7924; Lin, Peng/0000-0002-3567-701724123Pergamon-elsevier science ltdOxford</style></notes><auth-address><style face="normal" font="default" size="100%">Peking Univ, Coll Environm Sci, State Key Lab Environm Simulat &amp;amp; Pollut Control, Beijing 100871, Peoples R China.Hu, M (reprint author), Peking Univ, Coll Environm Sci, State Key Lab Environm Simulat &amp;amp; Pollut Control, Beijing 100871, Peoples R China.minhu@pku.edu.cn</style></auth-address></record></records></xml>