Formation of Denmark Strait overflow water and its hydro-chemical composition.

Tanhua, Toste , Olsson, K. Anders and Jeansson, Emil (2005) Formation of Denmark Strait overflow water and its hydro-chemical composition. Journal of Marine Systems, 57 (3-4). pp. 264-265. DOI 10.1016/j.jmarsys.2005.05.003.

[img] Text
tanhua.pdf - Published Version
Restricted to Registered users only

Download (1469Kb) | Contact

Supplementary data:

Abstract

The dense overflow across the Denmark Strait is investigated with hydrographic and hydro-chemical data and the water mass composition of the Denmark Strait Overflow Water (DSOW) is determined by multivariate analysis. Hydrographical properties, the transient tracers CFC-11 and CFC-12, oxygen and nutrients are utilized for the water mass definitions. Distribution and characteristics of water masses north of Denmark Strait are described, the important water masses at the sill and the variability on weekly time-scales are discussed, and the entrainment and mixing of water into the overflow plume in the northern Irminger Basin is calculated. The analysis indicates that water masses both from the Nordic Seas and the Arctic Ocean are important for the formation of DSOW. It is found that water masses transported with the East Greenland Current make up about 75% of the overflow at the sill. The overflow at, and shortly south of, the sill is inhomogeneous with a low-salinity component dominated by Polar Intermediate Water. The high-salinity component of the overflow is mainly of Arctic origin. The water mass composition, and the short-term variability for 7 repeats of sections close to the sill are described, and these illustrate that the overflow is in fact a composite of a number of water masses with different formation and transport histories. This indicate that the overflow is a robust feature, but that it responds to variations in the circulation or atmospheric forcing that influences the formation of intermediate and deep water masses within the Arctic Mediterranean and the North Atlantic. At a section about 400 km south of the sill the overflow is well mixed and modified by entrainment of, mainly, Iceland–Scotland Overflow Water and Labrador Sea Water, together constituting 30% of the overflow plume. The entrainment of Middle Irminger Water dominates shortly downstream of the sill, before the overflow plume reaches too deep but the entrainment seems to be intermittent in time.

Document Type: Article
Keywords: Oceanography; Chemistry; Aquaculture; Thermohaline circulation; Overflow; Water mixing; Freon tracers; Chemical properties; North Atlantic; Nordic Seas; Denmark Strait; 60–70°N; 20–40°W
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-CH Chemical Oceanography
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1016/j.jmarsys.2005.05.003
ISSN: 0924-7963
Projects: MAST
Date Deposited: 21 Jun 2010 10:18
Last Modified: 12 Jul 2017 12:35
URI: http://oceanrep.geomar.de/id/eprint/8534

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...