Effects of <sup>238</sup>U variability and physical transport on water column <sup>234</sup>Th downward fluxes in the coastal upwelling system off Peru
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Published:2020-10-14
Issue:19
Volume:17
Page:4919-4936
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Xie Ruifang C.ORCID, Le Moigne Frédéric A. C., Rapp Insa, Lüdke JanORCID, Gasser Beat, Dengler MarcusORCID, Liebetrau Volker, Achterberg Eric P.
Abstract
Abstract. The eastern boundary region of the southeastern Pacific Ocean hosts one of
the world's most dynamic and productive upwelling systems with an associated
oxygen minimum zone (OMZ). The variability in downward export fluxes in this
region, with strongly varying surface productivity, upwelling intensities
and water column oxygen content, is however poorly understood. Thorium-234
(234Th) is a powerful tracer to study the dynamics of export fluxes of
carbon and other elements, yet intense advection and diffusion in nearshore
environments impact the assessment of depth-integrated 234Th fluxes
when not properly evaluated. Here we use vessel-mounted acoustic Doppler current
profiler (VmADCP) current velocities,
satellite wind speed and in situ microstructure measurements to determine the
magnitude of advective and diffusive fluxes over the entire 234Th flux
budget at 25 stations from 11 to 16∘ S in the
Peruvian OMZ. Contrary to findings along the GEOTRACES P16 eastern section,
our results showed that weak surface wind speed during our cruises induced
low upwelling rates and minimal upwelled 234Th fluxes, whereas vertical
diffusive 234Th fluxes were important only at a few shallow shelf
stations. Horizontal advective and diffusive 234Th fluxes were
negligible because of small alongshore 234Th gradients. Our data
indicated a poor correlation between seawater 238U activity and
salinity. Assuming a linear relationship between the two would lead to
significant underestimations of the total 234Th flux by up to 40 % in
our study. Proper evaluation of both physical transport and variability in
238U activity is thus crucial in coastal 234Th flux studies.
Finally, we showed large temporal variations on 234Th residence times
across the Peruvian upwelling zone and cautioned future carbon export
studies to take these temporal variabilities into consideration while
evaluating carbon export efficiency.
Funder
Deutsche Forschungsgemeinschaft
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
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