Cardiff University | Prifysgol Caerdydd ORCA
Online Research @ Cardiff 
WelshClear Cookie - decide language by browser settings

Particle residence times in surface waters over the north-western Iberian Margin: comparison of pre-upwelling and winter periods

Schmidt, S., Chou, L. and Hall, Ian Robert 2002. Particle residence times in surface waters over the north-western Iberian Margin: comparison of pre-upwelling and winter periods. Journal of Marine Systems 32 (1-3) , pp. 3-11. 10.1016/S0924-7963(02)00027-1

Full text not available from this repository.

Abstract

Thorium-234 is used over the north-westernIberian Margin as a tracer of sinking particle fluxes on time scales of days to weeks. As a part of Ocean Margin Exchange (OMEX) project (II-II), samples were collected during pre-upwelling (June 1997) and winter (January 1998) periods. During the pre-upwelling situation, the distribution of total 234Th is rather uniform, with a mean deficiency of 24%. In contrast, particulate 234Th activities increase from the shelf to open ocean. As a result, particleresidencetimes derived from 234Th show a considerable range between 4 and 45 days, with a mean value of about 26 days. In the shelf waters, there is no clear trend in particleresidencetime, whereas the offshore stations present a more obvious signal with a gradual increase from about 10 days over the slope to nearly 30 days in the open ocean. In winter, total 234Th activities are more variable, and both deficit and equilibrium situations are observed. The mean deficit of total 234Th is low, about 10%, which may reflect reduced export fluxes at this time. Moreover, in the shelf waters during winter, particulate 234Th presents higher levels when compared with the pre-upwelling situation, which may be due to more intense resuspension of shallow sediments. As a consequence, average near-surfaceparticleresidencetimes are significantly longer in winter, with a mean value of 113 days. Estimates of export flux of particulate organic carbon (POC) from the upper ocean, using the ratio of POC and 234Th of particles, range between 1 and 56 mmol C m−2 day−1 in June 1997, and ca. 0 and 25 mmol C m−2 day−1 in January 1998. These variations reflect the large differences in hydrographic conditions and primary production levels between the two seasonal situations.

Item Type: Article
Date Type: Publication
Status: Published
Schools: Earth and Ocean Sciences
Subjects: G Geography. Anthropology. Recreation > GC Oceanography
Uncontrolled Keywords: Continental margin; Particle; Residencetime; Seasonal time scale; Th-234; Particulate organic carbon; NE Atlantic; Iberian Margin
Publisher: Elsevier
ISSN: 0924-7963
Last Modified: 04 Jun 2017 04:00
URI: http://orca.cf.ac.uk/id/eprint/30528

Citation Data

Cited 11 times in Google Scholar. View in Google Scholar

Cited 8 times in Scopus. View in Scopus. Powered By Scopus® Data

Cited 6 times in Web of Science. View in Web of Science.

Actions (repository staff only)

Edit Item Edit Item