Dominant role of eddies and filaments in the offshore transport of carbon and nutrients in the California Current System

Metadata Label Value
Author(s) Nagai, Takeyoshi, Gruber, Nicolas, Frenzel, Hartmut, Lachkar, Zouhair, McWilliams, James C., Plattner, Gian-Kasper
Publication Type Journal Items, Publication Status: Published
Full Text Search SFX for a Full-Text version of this document
Import to Mendeley Log in to provide feedback

Detailed Information

Metadata Field Content
Title Dominant role of eddies and filaments in the offshore transport of carbon and nutrients in the California Current System
Author(s) Nagai, Takeyoshi
Gruber, Nicolas
Frenzel, Hartmut
Lachkar, Zouhair
McWilliams, James C.
Plattner, Gian-Kasper
Journal or Series Title Journal of Geophysical Research C: Oceans
Volume Number 120
Issue Number 8
Start Page 5318
End Page 5341
ISSN 2169-9275
0148-0227
2169-9291
Publisher American Geophysical Union
Publication Place Washington, DC
Publication Date 2015-08
Abstract The coastal upwelling region of the California Current System (CalCS) is a well-known site of high productivity and lateral export of nutrients and organic matter, yet neither the magnitude nor the governing processes of this offshore transport are well quantified. Here we address this gap using a high-resolution (5 km) coupled physical-biogeochemical numerical simulation (ROMS). The results reveal (i) that the offshore transport is a very substantial component of any material budget in this region, (ii) that it reaches more than 800 km into the offshore domain, and (iii) that this transport is largely controlled by mesoscale processes, involving filaments and westward propagating eddies. The process starts in the nearshore areas, where nutrient and organic matter-rich upwelled waters pushed offshore by Ekman transport are subducted at the sharp lateral density gradients of upwelling fronts and filaments located at ∼25-100 km from the coast. The filaments are very effective in transporting the subducted material further offshore until they form eddies at their tips at about 100-200 km from the shore. The cyclonic eddies tend to trap the cold, nutrient, and organic matter-rich waters of the filaments, whereas the anticyclones formed nearby encapsulate the low nutrient and low organic matter waters around the filament. After their detachment, both types of eddies propagate further in offshore direction, with a speed similar to that of the first baroclinic mode Rossby waves, providing the key mechanism for long-range transport of nitrate and organic matter from the coast deep into the offshore environment.
DOI 10.1002/2015JC010889
Additional Notes Published online by Wiley
Received 31 March 2015, Accepted 21 June 2015, Accepted article online 24 June 2015, Published online 3 August 2015
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 004289352
Source Database ID SCOPUS-84941993718
WOS-000362653600003
Description File Name MIME Type Size
No details could be found
There are no links available for this record.
This record has not been viewed during this period

@article{Ng2015,
  author = "Nagai, Takeyoshi and Gruber, Nicolas and Frenzel, Hartmut and Lachkar, Zouhair and McWilliams, James C. and Plattner, Gian-Kasper",
  title = "{D}ominant role of eddies and filaments in the offshore transport of carbon and nutrients in the {C}alifornia {C}urrent {S}ystem",
  journal = "Journal of Geophysical Research C: Oceans",
  year = 2015,
  volume = "120",
  number = "8",
  pages = "5318--5341",
  month = aug,
}


E-Citations record created: Tue, 01 Sep 2015, 08:17:28 CET