GLORIA

GEOMAR Library Ocean Research Information Access

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Publication Date: 2023-12-09
    Description: In this work, we used field investigations in the Northwest Pacific Ocean and determined the surface seawater distributions of atmospheric non-methane hydrocarbons (NMHCs) and their oceanic sources. We conducted deck incubation experiments to investigate the responses of NMHCs to atmospheric aerosol deposition. The geographical distributions of NMHCs in seawater were related to ocean currents by controlling nutrient levels and phytoplankton biomasses and communities. The high nutrient levels caused by the Oyashio Current promoted the concentration of biogenic isoprene. In addition, the transformation of predominant phytoplankton also affected the isoprene formation. The increasing proportion of diatoms (68%) in the Oyashio Current and Kuroshio Extension contributed significantly to isoprene generation, and isoprene was 3-7 fold higher than that in other areas. Corresponding to seawater, the atmospheric NMHCs apart from isoprene displayed upward trends with increasing latitude. The deck incubation experiments revealed that the dynamic changes in phytoplankton biomass and community incurred by aerosol and acidic aerosol deposition were significantly accelerated isoprene production. However, no obvious responses of the other six NMHCs to atmospheric aerosol deposition were found in the incubation studies. Both ocean current movements and atmospheric deposition jointly influenced the generation and release of isoprene in the Northwest Pacific Ocean.
    Keywords: Aerosol deposition; Isoprene; Non-methane Hydrocarbons; Northwest Pacific Ocean; sea-to-air flux
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...