Relationships Between Supermicrometer Sea Salt Aerosol and Marine Boundary Layer Conditions: Insights From Repeated Identical Flight Patterns
Author
Schlosser, Joseph S.
Dadashazar, Hossein

Edwards, Eva‐Lou
Hossein Mardi, Ali
Prabhakar, Gouri
Stahl, Connor
Jonsson, Haflidi H.
Sorooshian, Armin
Affiliation
Univ Arizona, Dept Chem & Environm EngnDept Hydrol & Atmospher Sci
Issue Date
2020-05-25Keywords
MONterey Aerosol Research Campaign (MONARC)sea salt aerosol
EVS-3
wet scavenging
marine boundary layer
ACTIVATE
Metadata
Show full item recordPublisher
AMER GEOPHYSICAL UNIONCitation
Schlosser, J. S., Dadashazar, H., Edwards, E. L., Hossein Mardi, A., Prabhakar, G., Stahl, C., ... & Sorooshian, A. (2020). Relationships between supermicrometer sea salt aerosol and marine boundary layer conditions: insights from repeated identical flight patterns. Journal of Geophysical Research: Atmospheres, 125(12), e2019JD032346.Rights
© 2020. American Geophysical Union. All Rights Reserved.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
The MONterey Aerosol Research Campaign (MONARC) in May-June 2019 featured 14 repeated identical flights off the California coast over the open ocean at the same time each flight day. The objective of this study is to use MONARC data along with machine learning analysis to evaluate relationships between both supermicrometer sea salt aerosol number (N->1) and volume (V->1) concentrations and wind speed, wind direction, sea surface temperature (SST), ambient temperature (T-amb), turbulent kinetic energy (TKE), relative humidity (RH), marine boundary layer (MBL) depth, and drizzle rate. Selected findings from this study include the following: (i) Near surface (<60 m) N(>1)and V(>1)concentration ranges were 0.1-4.6 cm(-3)and 0.3-28.2 mu m(3) cm(-3), respectively; (ii) four meteorological regimes were identified during MONARC with each resulting in different N(>1)and V(>1)concentrations and also varying horizontal and vertical profiles; (iii) the relative predictive strength of the MBL properties varies depending on predicting N(>1)or V->1, with MBL depth being more highly ranked for predicting N(>1)and with TKE being higher for predicting V->1; (iv) MBL depths >400 m (<200 m) often correspond to lower (higher) N(>1)and V(>1)concentrations; (v) enhanced drizzle rates coincide with reduced N(>1)and V(>1)concentrations; (vi) N(>1)and V(>1)concentrations exhibit an overall negative relationship with SST and RH and an overall positive relationship with T-amb; and (vii) wind speed and direction were relatively weak predictors of N(>1)and V->1.Note
6 month embargo; first published online 25 May 2020ISSN
2169-897XEISSN
2169-8996Version
Final published versionSponsors
National Aeronautics and Space Administrationae974a485f413a2113503eed53cd6c53
10.1029/2019jd032346