You are in the accessibility menu

Please use this identifier to cite or link to this item: http://acervodigital.unesp.br/handle/11449/32237
Title: 
A comparison of global estimates of marine primary production from ocean color
Author(s): 
Institution: 
  • CALTECH
  • Old Dominion Univ
  • Fontier Res Ctr Global Change
  • Oceanog Lab
  • Stanford Univ
  • Tokyo Univ Informat Sci
  • Univ Paris 06
  • Duke Univ
  • Oregon State Univ
  • Univ Hawaii
  • Max Planck Inst Biogeochem
  • Univ New Hampshire
  • Universidade Estadual Paulista (UNESP)
  • Univ Connecticut
  • Joint Res Ctr
  • NOAA
  • NASA
  • Plymouth Marine Lab
  • Nagasaki Univ
  • Natl Res Inst Far Seas Fisheries
  • Univ E Anglia
  • British Antarctic Survey
  • Stennis Space Ctr
  • Lamont Doherty Earth Observ
  • Univ Calif Irvine
  • MBARI
  • Univ Roma Tor Vergata
  • Coll William & Mary
ISSN: 
0967-0645
Abstract: 
The third primary production algorithm round robin (PPARR3) compares output from 24 models that estimate depth-integrated primary production from satellite measurements of ocean color, as well as seven general circulation models (GCMs) coupled with ecosystem or biogeochemical models. Here we compare the global primary production fields corresponding to eight months of 1998 and 1999 as estimated from common input fields of photosynthetically-available radiation (PAR), sea-surface temperature (SST), mixed-layer depth, and chlorophyll concentration. We also quantify the sensitivity of the ocean-color-based models to perturbations in their input variables. The pair-wise correlation between ocean-color models was used to cluster them into groups or related output, which reflect the regions and environmental conditions under which they respond differently. The groups do not follow model complexity with regards to wavelength or depth dependence, though they are related to the manner in which temperature is used to parameterize photosynthesis. Global average PP varies by a factor of two between models. The models diverged the most for the Southern Ocean, SST under 10 degrees C, and chlorophyll concentration exceeding 1 mg Chlm(-3). Based on the conditions under which the model results diverge most, we conclude that current ocean-color-based models are challenged by high-nutrient low-chlorophyll conditions, and extreme temperatures or chlorophyll concentrations. The GCM-based models predict comparable primary production to those based on ocean color: they estimate higher values in the Southern Ocean, at low SST, and in the equatorial band, while they estimate lower values in eutrophic regions (probably because the area of high chlorophyll concentrations is smaller in the GCMs). Further progress in primary production modeling requires improved understanding of the effect of temperature on photosynthesis and better parameterization of the maximum photosynthetic rate. (c) 2006 Elsevier Ltd. All rights reserved.
Issue Date: 
1-Jan-2006
Citation: 
Deep-sea Research Part Ii-topical Studies In Oceanography. Oxford: Pergamon-Elsevier B.V., v. 53, n. 5-7, p. 741-770, 2006.
Time Duration: 
741-770
Publisher: 
Elsevier B.V.
Source: 
http://dx.doi.org/10.1016/j.dsr2.2006.01.028
URI: 
Access Rights: 
Acesso restrito
Type: 
outro
Source:
http://repositorio.unesp.br/handle/11449/32237
Appears in Collections:Artigos, TCCs, Teses e Dissertações da Unesp

There are no files associated with this item.
 

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.