Publications des scientifiques de l'IRD

Conte L., Szopa S., Aumont Olivier, Gros V., Bopp L. (2020). Sources and sinks of isoprene in the global open ocean : simulated patterns and emissions to the atmosphere. Journal of Geophysical Research : Oceans, 125 (9), p. e2019JC015946 [23 p.]. ISSN 2169-9275.

Titre du document
Sources and sinks of isoprene in the global open ocean : simulated patterns and emissions to the atmosphere
Année de publication
2020
Type de document
Article référencé dans le Web of Science WOS:000576619900040
Auteurs
Conte L., Szopa S., Aumont Olivier, Gros V., Bopp L.
Source
Journal of Geophysical Research : Oceans, 2020, 125 (9), p. e2019JC015946 [23 p.] ISSN 2169-9275
The ocean is a source of isoprene to the atmosphere. Although their global estimates are relatively low compared with the terrestrial source, these emissions have an influence on atmospheric chemistry. The lack of knowledge about the sources and sinks of isoprene in the ocean has hitherto precluded a precise assessment of when and where these emissions might be significant. Here we use the general circulation and biogeochemistry modelNucleus for European Modelling of the Ocean, Pelagic Interaction Scheme for Carbon and Ecosystem Studies(NEMO-PISCES) to explore different parameterizations of the 3D oceanic sources and sinks of isoprene. In addition, we investigate a representation of the isoprene emission due to photoproduction in the sea surface microlayer. Our model estimates are complemented by a new data compilation of laboratory isoprene production rates and in situ isoprene concentrations. This study constitutes the first attempt to simulate isoprene in a global 3D ocean biogeochemical model. We find that sea surface temperature is an important driver modulating phytoplankton isoprene production and that light levels only play a secondary role at the scale of the global ocean. Furthermore, the use of a variable biochemical consumption rate improves the model-data comparison. We show the importance of isoprene production below the mixed layer and, as a consequence, demonstrate that models based on 2D surface satellite chlorophyll-a could miss up to 18.5% of oceanic isoprene emissions. The oceanic isoprene emissions to the atmosphere are estimated to 0.66 (0.43-0.82) Tg C yr(-1)in the low range of previous estimates.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020] ; Limnologie physique / Océanographie physique [032]
Description Géographique
MONDE
Localisation
Fonds IRD [F B010079807]
Identifiant IRD
fdi:010079807
Contact