English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/15369
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

Title

Numerical simulations of submesoscale balanced vertical velocity forcing unsteady nutrient‐phytoplankton‐zooplankton distributions

AuthorsViúdez, Álvaro ; Claret, Mariona
KeywordsSubmesoscale NPZ dynamics
Numerical modeling
Vertical velocity forcing
NPZ
Issue Date30-Apr-2009
PublisherAmerican Geophysical Union
CitationJournal of Geophysical Research: Oceans 114(c4): C04023 (2009)
AbstractThe effect of submesoscale balanced (void of waves) vertical velocity on initially steady nutrient‐phytoplankton‐zooplankton (NPZ) distributions is investigated numerically. First, steady vertical NPZ profiles, continuous but not continuously differentiable at several depths, are found as analytical solutions to the NPZ equations in the absence of flow. These solutions admit numerical equivalents that are continuously differentiable in the numerical sense, here meaning convergence of the vertical derivative with respect to increasing vertical resolution. These NPZ solutions require, however, large vertical resolutions, with a grid size of few centimeters, to be properly discretisized. The ecological model is next coupled to a nonhydrostatic Boussinesq f plane physical model that explicitly conserves potential vorticity on isopycnals. Then the NPZ solutions are used as steady initial ecosystem conditions to investigate the role of submesoscale balanced vertical velocity in forcing NPZ anomalies in an idealized case of a baroclinic unstable jet. The results show that the baroclinic flow rapidly develops balanced vertical velocity that in turn favors NPZ anomalies. A large cancelation between the local change and the horizontal advection occurs in the ecosystem variables. This particularly occurs for zooplankton anomalies that therefore behave as better passive tracers of the horizontal flow than phytoplankton anomalies. However, once phytoplankton and zooplankton anomalies develop locally, forced by vertical velocity, they are horizontally advected away from the upwelling or downwelling regions so that spatial distributions of vertical velocity and ecological fields become eventually uncorrelated
Description14 pages, 14 figures, 2 tables, supporting information http://onlinelibrary.wiley.com/doi/10.1029/2008JC005172/suppinfo
Publisher version (URL)http://dx.doi.org/10.1029/2008JC005172
URIhttp://hdl.handle.net/10261/15369
DOI10.1029/2008JC005172
E-ISSN2169-9291
Appears in Collections:(ICM) Artículos
Files in This Item:
File Description SizeFormat 
Viudez_et_al_2009.pdf3,42 MBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 

Related articles:


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.