Logo image
The likelihood of observing dust-stimulated phytoplankton growth in waters proximal to the Australian continent
Journal article   Open access   Peer reviewed

The likelihood of observing dust-stimulated phytoplankton growth in waters proximal to the Australian continent

R A Cropp, A J Gabric, M Levasseur, G H McTainsh, A Bowie, C S Hassler, C S Law, H A McGowan, Neil W Tindale and R A Viscarra Rossel
Journal of Marine Systems, Vol.117-118, pp.43-52
2013
pdf
PDF - Author's Accepted Version (Open Access)1.14 MBDownloadView
Accepted Version PDF - Author Accepted Version (Open Access) Open Access CC BY-NC-ND V4.0
url
https://doi.org/10.1016/j.jmarsys.2013.02.013View
Published Version

Abstract

dust-phytoplankton link aeolian dust iron limitation Southern Ocean Tasman Sea Great Barrier Reef
We develop a tool to assist in identifying a link between naturally occurring aeolian dust deposition and phytoplankton response in the ocean. Rather than examining a single, or small number of dust deposition events, we take a climatological approach to estimate the likelihood of observing a definitive link between dust deposition and a phytoplankton bloom for the oceans proximal to the Australian continent. We use a dust storm index (DSI) to determine dust entrainment in the Lake Eyre Basin (LEB) and an ensemble of modelled atmospheric trajectories of dust transport from the basin, the major dust source in Australia. Deposition into the ocean is computed as a function of distance from the LEB source and the local over-ocean precipitation. The upper ocean's receptivity to nutrients, including dust-borne iron, is defined in terms of time-dependent, monthly climatological fields for light, mixed layer depth and chlorophyll concentration relative to the climatological monthly maximum. The resultant likelihood of a dust-phytoplankton link being observed is then mapped as a function of space and time. Our results suggest that the Southern Ocean (north of 45°S), the North West Shelf, and Great Barrier Reef are ocean regions where a rapid biological response to dust inputs is most likely to be observed. Conversely, due to asynchrony between deposition and ocean receptivity, direct causal links appear unlikely to be observed in the Tasman Sea and Southern Ocean south of 45°S.

Details

Metrics

108 File views/ downloads
935 Record Views

InCites Highlights

These are selected metrics from InCites Benchmarking & Analytics tool, related to this output

Collaboration types
Domestic collaboration
International collaboration
Web Of Science research areas
Geosciences, Multidisciplinary
Marine & Freshwater Biology
Oceanography

UN Sustainable Development Goals (SDGs)

This output has contributed to the advancement of the following goals:

#13 Climate Action
#14 Life Below Water

Source: InCites

Logo image