Implications of sea-ice biogeochemistry for oceanic production and emissions of dimethyl sulfide in the Arctic
Sea ice represents an additional oceanic source of the climatically active gas dimethyl sulfide (DMS) for the Arctic atmosphere. To what extent this source contributes to the dynamics of summertime Arctic clouds is, however, not known due to scarcity of field measurements. In this study, we devel...
Main Authors: | H. Hayashida, N. Steiner, A. Monahan, V. Galindo, M. Lizotte, M. Levasseur |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-06-01
|
Series: | Biogeosciences |
Online Access: | https://www.biogeosciences.net/14/3129/2017/bg-14-3129-2017.pdf |
Similar Items
-
Upward transport of bottom-ice dimethyl sulfide during advanced melting of arctic first-year sea ice
by: Margaux Gourdal, et al.
Published: (2019-08-01) -
Dimethyl sulfide dynamics in first-year sea ice melt ponds in the Canadian Arctic Archipelago
by: M. Gourdal, et al.
Published: (2018-05-01) -
CSIB v1 (Canadian Sea-ice Biogeochemistry): a sea-ice biogeochemical model for the NEMO community ocean modelling framework
by: H. Hayashida, et al.
Published: (2019-05-01) -
Increased oceanic dimethyl sulfide emissions in areas of sea ice retreat inferred from a Greenland ice core
by: Yutaka Kurosaki, et al.
Published: (2022-12-01) -
Ocean biogeochemistry in the coupled ocean–sea ice–biogeochemistry model FESOM2.1–REcoM3
by: Ö. Gürses, et al.
Published: (2023-08-01)