How well do global ocean biogeochemistry models simulate dissolved iron distributions?-Reference-Cited by-同舟云学术

How well do global ocean biogeochemistry models simulate dissolved iron distributions?

Published:2016-02 Issue:2 Volume:30 Page:149-174
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Tagliabue Alessandro¹,Aumont Olivier²,DeAth Ros³,Dunne John P.⁴,Dutkiewicz Stephanie⁵,Galbraith Eric⁶⁷,Misumi Kazuhiro⁸,Moore J. Keith⁹,Ridgwell Andy³¹⁰,Sherman Elliot⁹,Stock Charles⁴,Vichi Marcello¹¹¹²,Völker Christoph¹³,Yool Andrew¹⁴

Affiliation:

1. School of Environmental Sciences; University of Liverpool; Liverpool UK

2. IRD-LOCEAN; Institut Pierre Simon LaPlace; Paris France

3. School of Geographical Sciences; University of Bristol; Bristol UK

4. NOAA/Geophysical Fluid Dynamics Laboratory; Princeton New Jersey USA

5. Center for Global Change Science; Massachusetts Institute of Technology; Cambridge Massachussetts USA

6. Institució Catalana de Recerca i Estudis Avançats; Barcelona Spain

7. Institut de Ciència i Tecnologia Ambientals and Department of Mathematics; Universitat Autonoma de Barcelona; Barcelona Spain

8. Environmental Science Research Laboratory; Central Research Institute of Electric Power Industry; Abiko Japan

9. Department of Earth System Science; University of California; Irvine California USA

10. Department of Earth Sciences; University of California; Riverside California USA

11. Department of Oceanography; University of Cape Town; Cape Town South Africa

12. Nansen-Tutu Centre for Marine Environmental Research; Cape Town South Africa

13. Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung; Bremerhaven Germany

14. National Oceanography Centre; University of Southampton; Southampton UK

Funder

N8 consortium

Engineering and Physical Sciences Research Council

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Reference88 articles.

1. Chemical Tracers of Particle Transport

2. A model of the iron cycle in the ocean;Archer;Global Biogeochem. Cycles,2000

3. An ecosystem model of the global ocean including Fe, Si, P colimitations;Aumont;Global Biogeochem. Cycles,2003

4. PISCES-v2: An ocean biogeochemical model for carbon and ecosystem studies;Aumont;Geosci. Model Dev.,2015

5. Role of protozoan grazing in relieving iron limitation of phytoplankton;Barbeau;Nature,1996

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