Influence of the dry aerosol particle size distribution and morphology on the cloud condensation nuclei activation. An experimental and theoretical investigation
Junteng Wu et al.
Viewed
Total article views: 1,621 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,058
535
28
1,621
24
44
HTML: 1,058
PDF: 535
XML: 28
Total: 1,621
BibTeX: 24
EndNote: 44
Views and downloads (calculated since 22 Feb 2019)
Cumulative views and downloads
(calculated since 22 Feb 2019)
Total article views: 955 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
628
312
15
955
19
35
HTML: 628
PDF: 312
XML: 15
Total: 955
BibTeX: 19
EndNote: 35
Views and downloads (calculated since 08 Apr 2020)
Cumulative views and downloads
(calculated since 08 Apr 2020)
Total article views: 666 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
430
223
13
666
5
9
HTML: 430
PDF: 223
XML: 13
Total: 666
BibTeX: 5
EndNote: 9
Views and downloads (calculated since 22 Feb 2019)
Cumulative views and downloads
(calculated since 22 Feb 2019)
Viewed (geographical distribution)
Total article views: 1,600 (including HTML, PDF, and XML)
Thereof 1,596 with geography defined
and 4 with unknown origin.
Total article views: 969 (including HTML, PDF, and XML)
Thereof 967 with geography defined
and 2 with unknown origin.
Total article views: 631 (including HTML, PDF, and XML)
Thereof 629 with geography defined
and 2 with unknown origin.
Soot particles released during anthropogenic activities may lead to positive direct or negative indirect climate forcing depending on their aging in the atmosphere. The latter occurs whenever soot particles act as cloud condensation nuclei (CCN) and trigger the formation of persistent clouds. Herein, we investigate the impact of the size distribution and morphology of freshly emitted soot particles on their aging process and propose a model to quantitatively predict their efficiency as CCN.
Soot particles released during anthropogenic activities may lead to positive direct or negative...
