Abstract
Sea surface and atmospheric measurements of dimethylsulphide (DMS) were performed during the TransBrom cruise in the western Pacific Ocean between Japan and Australia in October 2009. Air-sea DMS fluxes were computed between 0 and 30 μmol m-2 d-1, which are in agreement with those computed by the current climatology, and peak emissions of marine DMS into the atmosphere were found during the occurrence of tropical storm systems. Atmospheric variability in DMS, however, did not f.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 8427-8437 |
| Number of pages | 11 |
| Journal | Atmospheric Chemistry and Physics |
| Volume | 13 |
| Issue number | 16 |
| DOIs | |
| State | Published - 2013 |
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ASJC Scopus subject areas
- Atmospheric Science
Cite this
Dimethylsulphide (DMS) emissions from the western Pacific Ocean : A potential marine source for stratospheric sulphur? / Marandino, C. A.; Tegtmeier, S.; Krüger, K.; Zindler, C.; Atlas, Elliot L; Moore, F.; Bange, H. W.
In: Atmospheric Chemistry and Physics, Vol. 13, No. 16, 2013, p. 8427-8437.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Dimethylsulphide (DMS) emissions from the western Pacific Ocean
T2 - A potential marine source for stratospheric sulphur?
AU - Marandino, C. A.
AU - Tegtmeier, S.
AU - Krüger, K.
AU - Zindler, C.
AU - Atlas, Elliot L
AU - Moore, F.
AU - Bange, H. W.
PY - 2013
Y1 - 2013
N2 - Sea surface and atmospheric measurements of dimethylsulphide (DMS) were performed during the TransBrom cruise in the western Pacific Ocean between Japan and Australia in October 2009. Air-sea DMS fluxes were computed between 0 and 30 μmol m-2 d-1, which are in agreement with those computed by the current climatology, and peak emissions of marine DMS into the atmosphere were found during the occurrence of tropical storm systems. Atmospheric variability in DMS, however, did not f.
AB - Sea surface and atmospheric measurements of dimethylsulphide (DMS) were performed during the TransBrom cruise in the western Pacific Ocean between Japan and Australia in October 2009. Air-sea DMS fluxes were computed between 0 and 30 μmol m-2 d-1, which are in agreement with those computed by the current climatology, and peak emissions of marine DMS into the atmosphere were found during the occurrence of tropical storm systems. Atmospheric variability in DMS, however, did not f.
UR - http://www.scopus.com/inward/record.url?scp=84883151469&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84883151469&partnerID=8YFLogxK
U2 - 10.5194/acp-13-8427-2013
DO - 10.5194/acp-13-8427-2013
M3 - Article
AN - SCOPUS:84883151469
VL - 13
SP - 8427
EP - 8437
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
SN - 1680-7316
IS - 16
ER -