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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 04003naa a2200613 4500 | |
| 001 | oai:DiVA.org:su-119072 | |
| 003 | SwePub | |
| 008 | 150727s2015 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1190722 URI |
| 024 | 7 | a https://doi.org/10.1002/2014JD0229632 DOI |
| 040 | a (SwePub)su | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a ref2 swepub-contenttype |
| 072 | 7 | a art2 swepub-publicationtype |
| 100 | 1 | a Modini, R. L.4 aut |
| 245 | 1 0 | a Primary marine aerosol-cloud interactions off the coast of California |
| 264 | 1 | c 2015 |
| 338 | a print2 rdacarrier | |
| 520 | a Primary marine aerosol (PMA)-cloud interactions off the coast of California were investigated using observations of marine aerosol, cloud condensation nuclei (CCN), and stratocumulus clouds during the Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) and the Stratocumulus Observations of Los-Angeles Emissions Derived Aerosol-Droplets (SOLEDAD) studies. Based on recently reported measurements of PMA size distributions, a constrained lognormal-mode-fitting procedure was devised to isolate PMA number size distributions from total aerosol size distributions and applied to E-PEACE measurements. During the 12 day E-PEACE cruise on the R/V Point Sur, PMA typically contributed less than 15% of total particle concentrations. PMA number concentrations averaged 12 cm(-3) during a relatively calmer period (average wind speed 12m/s(1)) lasting 8 days, and 71cm(-3) during a period of higher wind speeds (average 16m/s(1)) lasting 5 days. On average, PMA contributed less than 10% of total CCN at supersaturations up to 0.9% during the calmer period; however, during the higher wind speed period, PMA comprised 5-63% of CCN (average 16-28%) at supersaturations less than 0.3%. Sea salt was measured directly in the dried residuals of cloud droplets during the SOLEDAD study. The mass fractions of sea salt in the residuals averaged 12 to 24% during three cloud events. Comparing the marine stratocumulus clouds sampled in the two campaigns, measured peak supersaturations were 0.20.04% during E-PEACE and 0.05-0.1% during SOLEDAD. The available measurements show that cloud droplet number concentrations increased with >100 nm particles in E-PEACE but decreased in the three SOLEDAD cloud events. | |
| 650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskap0 (SwePub)1052 hsv//swe |
| 650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciences0 (SwePub)1052 hsv//eng |
| 653 | a sea spray aerosol | |
| 653 | a marine aerosol | |
| 653 | a cloud condensation nuclei | |
| 653 | a stratocumulus clouds | |
| 653 | a supersaturations | |
| 653 | a aerosol-cloud interactions | |
| 700 | 1 | a Frossard, A. A.4 aut |
| 700 | 1 | a Ahlm, L.4 aut |
| 700 | 1 | a Russell, L. M.4 aut |
| 700 | 1 | a Corrigan, C. E.4 aut |
| 700 | 1 | a Roberts, G. C.4 aut |
| 700 | 1 | a Hawkins, L. N.4 aut |
| 700 | 1 | a Schroder, J. C.4 aut |
| 700 | 1 | a Bertram, A. K.4 aut |
| 700 | 1 | a Zhao, R.4 aut |
| 700 | 1 | a Lee, A. K. Y.4 aut |
| 700 | 1 | a Abbatt, J. P. D.4 aut |
| 700 | 1 | a Lin, J.4 aut |
| 700 | 1 | a Nenes, A.4 aut |
| 700 | 1 | a Wang, Z.4 aut |
| 700 | 1 | a Wonaschuetz, A.4 aut |
| 700 | 1 | a Sorooshian, A.4 aut |
| 700 | 1 | a Noone, Kevin J.u Stockholms universitet,Institutionen för tillämpad miljövetenskap (ITM),Stockholm Univ, Dept Appl Environm Sci, S-10691 Stockholm, Sweden4 aut0 (Swepub:su)knoon |
| 700 | 1 | a Jonsson, H.4 aut |
| 700 | 1 | a Seinfeld, J. H.4 aut |
| 700 | 1 | a Toom-Sauntry, D.4 aut |
| 700 | 1 | a Macdonald, A. M.4 aut |
| 700 | 1 | a Leaitch, W. R.4 aut |
| 710 | 2 | a Stockholms universitetb Institutionen för tillämpad miljövetenskap (ITM)4 org |
| 773 | 0 | t Journal of Geophysical Research - Atmospheresg 120:9, s. 4282-4303q 120:9<4282-4303x 2169-897Xx 2169-8996 |
| 856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-119072 |
| 856 | 4 8 | u https://doi.org/10.1002/2014JD022963 |
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