What does temporal variability in aeolian dust deposition contribute to sea‐surface iron and chlorophyll distributions?
- 8 April 2008
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 35 (7)
- https://doi.org/10.1029/2007gl031131
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Decoupling of iron and phosphate in the global oceanGlobal Biogeochemical Cycles, 2005
- Modeling the speciation and biogeochemistry of iron at the Bermuda Atlantic Time‐series Study siteGlobal Biogeochemical Cycles, 2005
- Upper ocean ecosystem dynamics and iron cycling in a global three‐dimensional modelGlobal Biogeochemical Cycles, 2004
- An overview of the SeaWiFS project and strategies for producing a climate research quality global ocean bio-optical time seriesDeep Sea Research Part II: Topical Studies in Oceanography, 2004
- Propagation of climatic events on ocean stratification, marine biology, and CO2: Case studies over the 1979–1999 periodJournal of Geophysical Research: Oceans, 2003
- An ecosystem model of the global ocean including Fe, Si, P colimitationsGlobal Biogeochemical Cycles, 2003
- Seasonal and interannual variability of the mineral dust cycle under present and glacial climate conditionsJournal of Geophysical Research: Solid Earth, 2002
- A model of the iron cycle in the oceanGlobal Biogeochemical Cycles, 2000
- Iron supply and demand in the upper oceanGlobal Biogeochemical Cycles, 2000
- Atmospheric iron supply and enhanced vertical carbon flux in the NE subarctic Pacific: Is there a connection?Global Biogeochemical Cycles, 1998